Abstract
In this catalog, we present the results of a systematic study of gamma-ray bursts (GRBs) with reliable redshift estimates detected in the triggered mode of the Konus-Wind (KW) experiment during the period from 1997 February to 2016 June. The sample consists of 150 GRBs (including 12 short/hard bursts) and represents the largest set of cosmological GRBs studied to date over a broad energy band. From the temporal and spectral analyses of the sample, we provide the burst durations, the spectral lags, the results of spectral fits with two model functions, the total energy fluences, and the peak energy fluxes. Based on the GRB redshifts, which span the range , we estimate the rest-frame, isotropic-equivalent energy, and peak luminosity. For 32 GRBs with reasonably constrained jet breaks, we provide the collimation-corrected values of the energetics. We consider the behavior of the rest-frame GRB parameters in the hardness–duration and hardness–intensity planes, and confirm the "Amati" and "Yonetoku" relations for Type II GRBs. The correction for the jet collimation does not improve these correlations for the KW sample. We discuss the influence of instrumental selection effects on the GRB parameter distributions and estimate the KW GRB detection horizon, which extends to , stressing the importance of GRBs as probes of the early universe. Accounting for the instrumental bias, we estimate the KW GRB luminosity evolution, luminosity and isotropic-energy functions, and the evolution of the GRB formation rate, which are in general agreement with those obtained in previous studies.
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1. Introduction
Although decades have passed since the discovery of gamma-ray bursts (GRBs), many aspects of this astrophysical phenomenon remain unknown. The major breakthrough was achieved 20 years ago, when the first redshift was measured for the GRB 970508 (Metzger et al. 1997) and the cosmological nature of GRB sources was firmly established.
GRB redshifts are usually measured from the emission lines, the absorption features of the host galaxies imposed on the afterglow continuum, or photometrically. However, there are other approaches to estimate redshifts, e.g., the "pseudo-redshift" (pseudo-z) technique based on the spectral properties of GRB prompt high energy emission (Atteia 2003) or searching for a minimum on the intrinsic hydrogen column density versus redshift plane (see, e.g., Ghisellini et al. 1999). Considering only spectroscopic and photometric redshifts there were ∼450 GRBs with reliably measured redshifts by the middle of 2016. As of 2016, the GRB redshifts fill a range from spectroscopic (GRB 980425; Foley et al. 2006) to photometric (GRB 090429B; Cucchiara et al. 2011) or NIR spectroscopic (GRB 090423; Salvaterra et al. 2009); however, they are expected to occur and be detectable out to redshifts greater than and possibly up to z ≈ 15–20 (Lamb & Reichart 2001).
The explosion energetics is one of the key parameters for understanding the GRB progenitors and the GRB central engine physics. Knowing a GRB redshift one can estimate the isotropic equivalent gamma-ray energy () as a substitute for the energy released by the central engine. Huge isotropic energy releases up to erg (e.g., GRB 080916C has erg at Abdo et al. 2009; Greiner et al. 2009) were first explained for the GRB 970508 (Waxman et al. 1998) by taking into account jet beaming: correction for the jet collimation decreases the energy release and peak luminosity of GRBs by orders of magnitude. The hypothesis that GRBs are non-spherical explosions implies that, when the tightly collimated relativistic fireball is decelerated by the circumburst medium (CBM) down to the Lorentz factor (where is the jet opening angle), an achromatic break (jet break) should appear, in the form of a sudden steepening in the GRB afterglow light curve, at a characteristic time . Knowing , the jet opening angle can be estimated (Rhoads 1997; Sari et al. 1999) and the collimation-corrected GRB energy calculated. With typical collimation angles of a few degrees, the true energy release from most GRBs is erg, on par with that of a supernova (Frail et al. 2001).
The Konus-Wind (hereafter KW; Aptekar et al. 1995) experiment has operated since 1994 November and plays an important role in the GRB studies thanks to its unique set of characteristics: the spacecraft orbits in interplanetary space that provides an exceptionally stable background and continuous coverage of the full sky by two omnidirectional NaI detectors, high temporal resolution, and the wide energy range of the detectors (∼10 keV–10 MeV, nominally). KW has triggered ∼4350 times on a variety of transient events, including ∼2700 GRBs, up to 2016 June; thus KW has been detecting GRBs at a rate of events per year. Being a part of the Interplanetary Network (IPN), KW is enabling GRB localizations to be constrained by triangulation (see, e.g., Pal'shin et al. 2013 and Hurley et al. 2013 for details).
Thanks to the wide energy range, the GRB spectral cutoff energy (parameterized as , the maximum of spectrum) can be derived directly from the KW data and the GRB energetics can be estimated using fewer extrapolations. Coupled with well-measured redshifts, the accurate estimates of these parameters provide an excellent testing ground for widely discussed correlations between rest-frame spectral hardness and energetics, e.g., the "Amati" (Amati et al. 2002), "Yonetoku" (Yonetoku et al. 2004) or "Ghirlanda" (Ghirlanda et al. 2004) relations. This could facilitate using GRBs as standard candles (see, e.g., Atteia 1997 or Friedman & Bloom 2005) and probing cosmological parameters with GRBs (see, e.g., Cohen & Piran 1997 or Diaferio et al. 2011).
Here, we present a complete sample of GRBs with reliably measured redshifts that triggered KW from 1997 February to 2016 June. The sample consists of 150 bursts and represents the largest set of GRBs with known redshifts detected by a single instrument over a wide energy range. The KW bursts observed in the waiting mode will be presented in a forthcoming catalog (A. Tsvetkova et al. 2017, in preparation) We start this catalog with a brief description of the KW instrument in Section 2. The burst sample is described in Section 3. In Section 4 we present the temporal and spectral analyses of the sample, and the derived observer- and rest-frame energetics. In Section 5 we discuss the derived prompt emission parameters, the KW-specific instrumental biases, and the rest-frame properties of the KW GRBs.
All the errors quoted in this catalog are at the 68% confidence level (CL) and are of a statistical nature only. Throughout the paper, we assume the standard ΛCDM model: km s−1 Mpc−1, , and (Planck Collaboration et al. 2014). We also adopt the conventional notation .
2. Instrumentation
KW is a gamma-ray spectrometer designed to study temporal and spectral characteristics of GRBs, solar flares, soft gamma repeater bursts, and other transient phenomena over a wide energy range from 13 keV to 10 MeV, nominally (i.e., at launch; see the end of this section). It consists of two identical omnidirectional NaI(Tl) detectors, mounted on opposite faces of the rotationally stabilized Wind spacecraft. One detector (S1) points toward the south ecliptic pole, thereby observing the south ecliptic hemisphere; the other (S2) observes the north ecliptic hemisphere. Each detector has an effective area of ∼80–160 , depending on the photon energy and incident angle.
In interplanetary space far outside the Earth's magnetosphere, KW has the advantages over Earth-orbiting GRB monitors of continuous coverage, uninterrupted by Earth occultation, and a steady background, undistorted by passages through Earth's trapped radiation, and subject only to occasional solar particle events. The Wind distance from Earth as a function of time is presented in Pal'shin et al. (2013); it ranges up to 5.5 lt-s.
The instrument has two operational modes: waiting and triggered. While in the waiting mode, the count rates are recorded in three energy windows G1 (13–50 keV), G2 (50–200 keV), and G3 (200–760 keV) with 2.944 s time resolution. When the count rate in the G2 window exceeds a threshold above the background on one of two fixed timescales , 1 s or 140 ms, the instrument switches into the triggered mode, for which the waiting-mode data are also available up to T0+250 s. In the triggered mode, the count rates in the three energy windows are recorded with time resolutions varying from 2 ms up to 256 ms. These time histories, with a total duration of ∼230 s, also include 0.512 s of pre-trigger history. Spectral measurements are carried out, starting from the trigger time T0, in two overlapping energy intervals, PHA1 (13–760 keV) and PHA2 (160 keV–10 MeV), with 64 spectra being recorded for each interval over a 63-channel, pseudo-logarithmic, energy scale. The first four spectra are measured with a fixed accumulation time of 64 ms in order to study short bursts. For the subsequent 52 spectra, an adaptive system determines the accumulation times, which may vary from 0.256 to 8.192 s depending on the current count rate in the G2 window. The last 8 spectra are obtained for 8.192 s each. As a result the minimum duration of spectral measurements is 79.104 s, and the maximum is 491.776 s (which is ∼260 s longer than the time history duration). After the triggered-mode measurements are finished, KW switches into the data-readout mode for ∼1 hr and no measurements are available for this time interval.
For all the bursts, we used a standard KW dead time (DT) correction procedure for light curves (with a DT of a few μs) and spectra (with a DT of ∼42 μs). The detector response matrix (DRM), which is a function only of the burst angle relative to the instrument axis, was computed using the GEANT4 package (Agostinelli et al. 2003). The detailed description of the instrument response calculation is presented in Terekhov et al. (1998). The latest version of the DRM contains responses calculated for 264 photon energies between 5 keV and 30 MeV on a quasi-logarithmic scale for incident angles from to with a step of . The energy scale is calibrated in flight using the 1460 keV line of 40K and the 511 keV e+e− annihilation line. The gain of the detectors has slowly decreased during the long period of operation. The instrumental control of the gain became non-functional in 1997 and the spectral range changed to 25 keV–18 MeV for the S1 detector and to 20 keV–15 MeV for the S2 detector, from the original 13 keV–10 MeV; the G1, G2, G3, PHA1, and PHA2 energy bounds shifted accordingly.
The consistency of the KW spectral parameters and those obtained in other GRB experiments was verified by a cross-calibration with Swift-BAT and Suzaku-WAM (Sakamoto et al. 2011b), and in joint spectral fits with Fermi-GBM (e.g., Lipunov et al. 2016). It was shown that the difference in the spectrum normalization between KW and these instruments is % in joint fits. A more detailed discussion of the KW instrumental issues can be found in Svinkin et al. (2016b), hereafter S16.
3. The Burst Sample
The sample contains 150 GRBs with reliable redshift estimates detected by KW in the triggered mode from the beginning of the afterglow era in 1997 to the middle of 2016. The general information about these bursts is presented in Table 1. The first three columns contain the GRB name as provided in the Gamma-ray Burst Coordinates Network circulars,6 the KW trigger time T0, and the KW trigger time corrected for the burst front propagation from Wind to the Earth center (the geocenter time).
Table 1. General Information
Burst | Trigger | Geocenter | Type | Local. | Local. | Otherc | Det. | Inc. angle | z | z typed | z |
---|---|---|---|---|---|---|---|---|---|---|---|
Name | Time | Time | instr. | References | obs. | (deg) | References | ||||
GRB 970228 | 02:58:01.317 | 02:58:01.263 | II | BeppoSAX | (1) | 3 | S1 | 79.1 | 0.695 | s | (2) |
GRB 970828 | 17:44:42.357 | 17:44:42.157 | II | RXTEASM | (3) | ⋯ | S2 | 7.1 | 0.9578a | s | (4) |
GRB 971214 | 23:20:52.214 | 23:20:51.043 | II | BeppoSAX | (1) | 1 3 | S2 | 33.9 | 3.418 | s | (5) |
GRB 990123 | 09:47:14.151 | 09:47:15.040 | II | BeppoSAX | (1) | 1 3 | S2 | 29.9 | 1.6004 | s | (6) |
GRB 990506 | 11:23:30.813 | 11:23:31.274 | II | BeppoSAX | (1) | 1 3 | S1 | 65.1 | 1.30658a | s | (7) |
GRB 990510 | 08:49:10.059 | 08:49:10.052 | II | BeppoSAX | (1) | 1 3 | S1 | 28.7 | 1.6187 | s | (8) |
GRB 990705 | 16:01:26.864 | 16:01:26.352 | II | BeppoSAX | (1) | 3 | S1 | 7.1 | 0.8424 | s | (9) |
GRB 990712 | 16:43:06.123 | 16:43:03.763 | II | BeppoSAX | (1) | 3 | S1 | 33.2 | 0.4331 | s | (8) |
GRB 991208 | 04:36:53.263 | 04:36:53.224 | II | IPN | (10) | ⋯ | S2 | 23.0 | 0.7055 | s | (11) |
GRB 991216 | 16:07:18.085 | 16:07:18.535 | II | BeppoSAX | (1) | 1 3 | S1 | 78.1 | 1.02 | s | (12) |
GRB 000131 | 14:59:15.102 | 14:59:14.388 | II | IPN | (13) | ⋯ | S1 | 14.7 | 4.5 | s | (14) |
GRB 000210 | 08:44:05.712 | 08:44:06.695 | II | BeppoSAX | (1) | 3 | S1 | 41.6 | 0.8463a | s | (15) |
GRB 000301C | 09:51:38.569 | 09:51:37.589 | II | IPN+ASM | (16) | ⋯ | S2 | 40.1 | 2.0335 | s | (17) |
GRB 000418 | 09:53:09.906 | 09:53:08.258 | II | IPN | (18) | ⋯ | S2 | 69.1 | 1.1181 | s | (7) |
GRB 000911 | 07:15:25.914 | 07:15:28.816 | II | IPN | (19) | ⋯ | S1 | 84.3 | 1.0585 | s | (20) |
GRB 000926 | 23:49:33.661 | 23:49:32.447 | II | IPN | (21) | ⋯ | S2 | 16.3 | 2.0369 | s | (22) |
GRB 010222 | 07:23:11.652 | 07:23:12.337 | II | BeppoSAX | (1) | 3 | S2 | 34.5 | 1.4768 | s | (23) |
GRB 010921 | 05:15:57.151 | 05:15:56.112 | II | BeppoSAX | (1) | 2 3 | S2 | 44.6 | 0.45 | s | (24) |
GRB 011121 | 18:47:13.457 | 18:47:13.448 | II | BeppoSAX | (1) | 3 | S1 | 25.7 | 0.36 | s | (25) |
GRB 020405 | 00:41:39.501 | 00:41:37.640 | II | BeppoSAX | (1) | 3 | S1 | 71.9 | 0.6898 | s | (26) |
GRB 020813 | 02:44:40.651 | 02:44:40.139 | II | HETE-2 | (27) | 2 | S1 | 91.6 | 1.254 | s | (28) |
GRB 020819Be | 14:57:39.766 | 14:57:38.125 | II | HETE-2 | (27) | 2 | S2 | 81.0 | 0.411a | s | (29) |
GRB 021211 | 11:18:35.206 | 11:18:34.494 | II | HETE-2 | (30) | 2 | S1 | 76.9 | 1.004 | s | (31) |
GRB 030329 | 11:37:29.254 | 11:37:26.378 | II | HETE-2 | (27) | 2 | S2 | 77.5 | 0.16854 | s | (32) |
GRB 040924 | 11:52:15.280 | 11:52:12.600 | II | HETE-2 | (33) | 2 | S2 | 87.0 | 0.859 | s | (34) |
GRB 041006 | 12:18:43.030 | 12:18:39.061 | II | HETE-2 | (35) | 2 | S2 | 94.3 | 0.716 | s | (36) |
GRB 050401 | 14:20:11.344 | 14:20:09.710 | II | SwiftBAT | (37) | 4 | S2 | 66.2 | 2.8992b | s | (38) |
GRB 050525A | 00:02:56.704 | 00:02:53.543 | II | SwiftBAT | (37) | 4 | S2 | 40.5 | 0.606 | s | (39) |
GRB 050603 | 06:29:00.767 | 06:29:02.176 | II | SwiftBAT | (37) | 4 | S1 | 51.6 | 2.821 | s | (40) |
GRB 050820Af | 06:39:14.512 | 06:39:10.966 | II | SwiftBAT | (37) | 4 | S2 | 63.2 | 2.6147 | s | (41) |
GRB 050922C | 19:55:54.480 | 19:55:50.299 | II | SwiftBAT | (37) | 2 4 | S2 | 82.7 | 2.198 | s | (42) |
GRB 051008 | 16:33:20.762 | 16:33:23.339 | II | SwiftBAT | (37) | 4 | S2 | 43.1 | 2.77a g | p | (43) |
GRB 051022 | 13:08:25.298 | 13:08:21.749 | II | HETE-2 | (27) | 2 | S2 | 71.7 | 0.8 | s | (44) |
GRB 051109A | 01:12:22.541 | 01:12:21.735 | II | SwiftBAT | (37) | 4 | S2 | 41.5 | 2.346 | s | (45) |
GRB 051221A | 01:51:12.976 | 01:51:15.938 | I | SwiftBAT | (37) | 4 | S2 | 62.3 | 0.5465 | s | (46) |
GRB 060121 | 22:25:00.890 | 22:24:56.407 | IIh | HETE-2 | (47) | 2 | S2 | 62.1 | 4.6i | p | (48) |
GRB 060124 | 16:04:13.894 | 16:04:10.869 | II | SwiftBAT | (37) | 4 | S2 | 43.4 | 2.3000 | s | (49) |
GRB 060502A | 03:03:33.119 | 03:03:32.793 | II | SwiftBAT | (37) | 4 | S2 | 11.4 | 1.5026 | s | (49) |
GRB 060614 | 12:43:51.590 | 12:43:47.332 | IIj | SwiftBAT | (37) | 4 | S1 | 54.4 | 0.1254 | s | (50) |
GRB 060814 | 23:02:34.447 | 23:02:34.295 | II | SwiftBAT | (37) | 4 | S2 | 55.3 | 1.9229a | s | (51) |
GRB 060912A | 13:55:57.788 | 13:55:54.482 | II | SwiftBAT | (37) | 4 | S2 | 72.9 | 0.937 | s | (52) |
GRB 061006 | 16:45:26.896 | 16:45:27.817 | Ik | SwiftBAT | (37) | 4 | S1 | 13.9 | 0.4377 | s | (53) |
GRB 061007 | 10:08:09.344 | 10:08:07.767 | II | SwiftBAT | (37) | 4 | S1 | 27.0 | 1.2622 | s | (49) |
GRB 061021 | 15:39:08.304 | 15:39:09.770 | II | SwiftBAT | (37) | 4 | S1 | 56.4 | 0.3453 | s | (54) |
GRB 061121 | 15:23:32.445 | 15:23:30.905 | II | SwiftBAT | (37) | 4 | S1 | 65.2 | 1.3145 | s | (49) |
GRB 061201 | 15:58:34.558 | 15:58:36.886 | I | SwiftBAT | (37) | 4 | S1 | 33.4 | 0.111 | s | (55) |
GRB 061222A | 03:30:14.682 | 03:30:13.937 | II | SwiftBAT | (37) | 4 | S2 | 47.6 | 2.088a | s | (56) |
GRB 070125 | 07:20:50.853 | 07:20:45.664 | II | IPN+BAT | (57) | ⋯ | S2 | 80.0 | 1.547 | s | (58) |
GRB 070328 | 03:53:49.993 | 03:53:52.064 | II | SwiftBAT | (37) | 4 | S1 | 35.6 | 2.0627 | s | (54) |
GRB 070508 | 04:18:22.779 | 04:18:20.346 | II | SwiftBAT | (37) | 4 | S1 | 32.9 | 0.82b | s | (59) |
GRB 070521 | 06:51:31.587 | 06:51:28.779 | II | SwiftBAT | (37) | 4 | S2 | 39.9 | 1.7a l | p | (60) |
GRB 070714B | 04:59:25.178 | 04:59:29.705 | I | SwiftBAT | (37) | 4 | S1 | 97.9 | 0.923 | s | (61) |
GRB 071003 | 07:40:55.120 | 07:40:53.830 | II | SwiftBAT | (37) | 4 | S2 | 59.6 | 1.60435 | s | (62) |
GRB 071010B | 20:45:48.490 | 20:45:49.125 | II | SwiftBAT | (37) | 4 | S2 | 58.6 | 0.947 | s | (63) |
GRB 071020 | 07:02:26.637 | 07:02:24.778 | II | SwiftBAT | (37) | 4 | S2 | 78.0 | 2.1462 | s | (49) |
GRB 071112C | 18:33:02.583 | 18:32:58.044 | II | SwiftBAT | (64) | 4 | S1 | 102.4 | 0.8227 | s | (49) |
GRB 071117 | 14:50:04.535 | 14:50:06.512 | II | SwiftBAT | (37) | 4 | S1 | 41.8 | 1.3308 | s | (49) |
GRB 071227 | 20:13:48.722 | 20:13:47.668 | I | SwiftBAT | (37) | 4 | S1 | 18.3 | 0.384 | s | (65) |
GRB 080319B | 06:12:50.339 | 06:12:47.321 | II | SwiftBAT | (37) | 4 | S2 | 42.3 | 0.9382 | s | (49) |
GRB 080319C | 12:25:57.938 | 12:25:57.035 | II | SwiftBAT | (37) | 4 | S2 | 12.3 | 1.9492b | s | (49) |
GRB 080411 | 21:15:32.496 | 21:15:32.853 | II | SwiftBAT | (37) | 4 | S1 | 18.6 | 1.0301 | s | (49) |
GRB 080413A | 02:54:23.605 | 02:54:21.182 | II | SwiftBAT | (37) | 4 | S2 | 95.1 | 2.433 | s | (49) |
GRB 080413B | 08:51:11.831 | 08:51:12.288 | II | SwiftBAT | (37) | 4 | S2 | 96.0 | 1.1014 | s | (49) |
GRB 080514B | 09:55:58.672 | 09:55:57.137 | II | SuperAGILE/IPN | (66) | 4 | S2 | 75.4 | 1.8 | p | (67) |
GRB 080602 | 01:31:26.229 | 01:31:28.289 | II | SwiftBAT | (37) | 4 | S1 | 74.0 | 1.8204 | s | (54) |
GRB 080603B | 19:38:12.383 | 19:38:14.633 | II | SwiftBAT | (37) | 4 | S2 | 32.6 | 2.6892 | s | (49) |
GRB 080605 | 23:48:02.336 | 23:47:57.581 | II | SwiftBAT | (37) | 4 | S2 | 62.8 | 1.6403b | s | (49) |
GRB 080607 | 06:07:23.336 | 06:07:22.085 | II | SwiftBAT | (37) | 4 | S2 | 69.5 | 3.0363b | s | (68) |
GRB 080721 | 10:25:10.927 | 10:25:07.575 | II | SwiftBAT | (37) | 4 | S2 | 85.0 | 2.591 | s | (69) |
GRB 080916C | 00:12:44.632 | 00:12:46.223 | II | FermiLAT | (70) | 5 6 | S1 | 17.1 | 4.35m | p | (71) |
GRB 080916A | 09:45:21.715 | 09:45:19.813 | II | SwiftBAT | (37) | 4 5 | S1 | 47.0 | 0.6887 | s | (49) |
GRB 081121 | 20:35:31.435 | 20:35:30.430 | II | SwiftBAT | (37) | 4 5 | S1 | 5.9 | 2.512 | s | (72) |
GRB 081203A | 13:51:30.368 | 13:51:31.069 | II | SwiftBAT | (37) | 4 | S2 | 15.6 | 2.05 | s | (73) |
GRB 081221 | 16:21:14.915 | 16:21:13.479 | II | SwiftBAT | (37) | 4 5 | S1 | 61.3 | 2.26 | s | (74) |
GRB 081222 | 04:54:02.534 | 04:54:01.179 | II | SwiftBAT | (37) | 4 5 | S1 | 50.1 | 2.77 | s | (75) |
GRB 090102 | 02:55:36.283 | 02:55:32.211 | II | SwiftBAT | (37) | 4 5 | S2 | 76.2 | 1.547 | s | (76) |
GRB 090201 | 17:47:00.275 | 17:46:58.787 | II | SwiftBAT | (37) | 4 | S1 | 20.0 | 2.1000 | s | (54) |
GRB 090323 | 00:02:54.632 | 00:02:50.491 | II | FermiLAT | (70) | 5 6 | S2 | 70.1 | 3.6 | s | (77) |
GRB 090328 | 09:36:49.486 | 09:36:50.556 | II | FermiLAT | (70) | 5 6 | S1 | 24.6 | 0.736 | s | (78) |
GRB 090424 | 14:12:11.725 | 14:12:08.925 | II | SwiftBAT | (37) | 4 5 | S2 | 70.8 | 0.544 | s | (79) |
GRB 090510 | 00:23:01.547 | 00:23:00.536 | I | SwiftBAT | (37) | 4 5 6 | S1 | 75.4 | 0.903 | s | (80) |
GRB 090618 | 08:28:24.974 | 08:28:26.755 | II | SwiftBAT | (37) | 4 5 | S2 | 13.6 | 0.54 | s | (81) |
GRB 090709A | 07:38:34.965 | 07:38:34.873 | II | SwiftBAT | (37) | 4 | S2 | 10.5 | 1.8a n | p | (60) |
GRB 090715B | 21:03:19.008 | 21:03:18.138 | II | SwiftBAT | (37) | 4 | S2 | 23.9 | 3.00 | s | (82) |
GRB 090812 | 06:02:38.942 | 06:02:35.958 | II | SwiftBAT | (37) | 4 | S1 | 83.0 | 2.452 | s | (83) |
GRB 090926A | 04:20:28.683 | 04:20:27.945 | II | FermiLAT | (70) | 5 6 | S1 | 36.0 | 2.1062 | s | (84) |
GRB 091003 | 04:35:43.801 | 04:35:45.946 | II | FermiLAT | (70) | 5 6 | S2 | 31.3 | 0.8969 | s | (85) |
GRB 091020 | 21:36:44.860 | 21:36:45.632 | II | SwiftBAT | (64) | 4 5 | S2 | 46.1 | 1.71 | s | (86) |
GRB 091117A | 17:44:29.513 | 17:44:25.673 | I | SwiftBAT | (87) | 4 | S1 | 62.4 | 0.096 | s | (88) |
GRB 091127 | 23:25:49.449 | 23:25:45.602 | II | SwiftBAT | (64) | 4 5 | S1 | 58.5 | 0.49034 | s | (89) |
GRB 100206A | 13:30:06.775 | 13:30:05.433 | I | SwiftBAT | (64) | 4 5 | S1 | 85.7 | 0.41 | s | (90) |
GRB 100414A | 02:20:27.289 | 02:20:23.328 | II | FermiLAT | (70) | 4 5 6 | S2 | 77.2 | 1.368 | s | (91) |
GRB 100606A | 19:12:43.712 | 19:12:42.046 | II | SwiftBAT | (64) | 4 | S1 | 35.6 | 1.5545 | s | (54) |
GRB 100621A | 03:03:33.352 | 03:03:30.209 | II | SwiftBAT | (64) | 4 | S1 | 57.4 | 0.542 | s | (92) |
GRB 100728A | 02:18:20.008 | 02:18:24.502 | II | SwiftBAT | (64) | 4 5 6 | S1 | 51.3 | 1.567 | s | (93) |
GRB 100814A | 03:50:11.288 | 03:50:09.556 | II | SwiftBAT | (64) | 4 5 | S1 | 64.7 | 1.44 | s | (94) |
GRB 100816A | 00:37:53.983 | 00:37:51.215 | II | SwiftBAT | (64) | 4 5 | S2 | 62.5 | 0.8049 | s | (95) |
GRB 100906A | 13:49:30.732 | 13:49:28.387 | II | SwiftBAT | (64) | 4 5 | S2 | 49.5 | 1.727 | s | (96) |
GRB 101213A | 10:49:18.472 | 10:49:22.676 | II | SwiftBAT | (64) | 4 5 | S2 | 48.2 | 0.414 | s | (97) |
GRB 101219A | 02:31:34.716 | 02:31:29.786 | I | SwiftBAT | (64) | 4 | S1 | 64.9 | 0.718 | s | (98) |
GRB 110213A | 05:17:28.893 | 05:17:28.492 | II | SwiftBAT | (64) | 4 5 | S2 | 58.8 | 1.46 | s | (99) |
GRB 110422A | 15:41:42.948 | 15:41:45.300 | II | SwiftBAT | (64) | 4 | S2 | 37.7 | 1.77 | s | (100) |
GRB 110503A | 17:35:41.862 | 17:35:43.747 | II | SwiftBAT | (64) | 4 | S2 | 56.9 | 1.613 | s | (101) |
GRB 110715A | 13:13:55.304 | 13:13:51.418 | II | SwiftBAT | (64) | 4 | S1 | 64.5 | 0.82 | s | (102) |
GRB 110731A | 11:09:34.604 | 11:09:30.409 | II | SwiftBAT | (64) | 4 5 6 | S1 | 84.6 | 2.83 | s | (103) |
GRB 110918A | 21:27:02.856 | 21:26:58.937 | II | IPN | (104) | ⋯ | S1 | 52.3 | 0.984 | s | (105) |
GRB 111008A | 22:13:01.676 | 22:12:58.248 | II | SwiftBAT | (64) | 4 | S1 | 38.1 | 5.0 | s | (106) |
GRB 111228A | 15:45:36.171 | 15:45:34.790 | II | SwiftBAT | (64) | 4 5 | S2 | 84.3 | 0.7156 | s | (107) |
GRB 120119A | 04:04:34.872 | 04:04:31.459 | II | SwiftBAT | (64) | 4 5 | S1 | 61.0 | 1.728 | s | (108) |
GRB 120624B | 22:20:06.904 | 22:20:06.153 | II | SwiftBAT | (64) | 4 5 6 | S2 | 85.4 | 2.1974 | s | (109) |
GRB 120711A | 02:45:55.810 | 02:45:55.657 | II | INTEGRAL | (110) | 5 6 | S1 | 4.8 | 1.405 | s | (111) |
GRB 120716A | 17:05:07.357 | 17:05:04.087 | II | IPN | (112) | 5 | S2 | 64.0 | 2.486 | s | (113) |
GRB 120804A | 00:54:15.749 | 00:54:14.794 | II | SwiftBAT | (64) | 4 | S2 | 99.2 | 1.3 | p | (114) |
GRB 121128A | 05:05:53.703 | 05:05:53.474 | II | SwiftBAT | (64) | 4 5 | S2 | 19.1 | 2.2 | s | (115) |
GRB 130408A | 21:51:41.194 | 21:51:38.956 | II | SwiftBAT | (64) | 4 | S1 | 43.0 | 3.758 | s | (116) |
GRB 130427A | 07:47:09.501 | 07:47:06.468 | II | SwiftBAT | (64) | 4 5 6 | S2 | 67.4 | 0.3399 | s | (117) |
GRB 130505A | 08:22:27.038 | 08:22:26.527 | II | SwiftBAT | (64) | 4 | S1 | 91.0 | 2.27 | s | (118) |
GRB 130518A | 13:54:57.501 | 13:55:01.478 | II | SwiftBAT | (64) | 4 5 6 | S2 | 45.9 | 2.488 | s | (119) |
GRB 130603B | 15:49:16.448 | 15:49:14.164 | I | SwiftBAT | (64) | 4 | S2 | 77.4 | 0.3565 | s | (120) |
GRB 130701A | 04:17:42.161 | 04:17:43.592 | II | SwiftBAT | (64) | 4 | S2 | 56.2 | 1.155 | s | (121) |
GRB 130831A | 13:04:22.044 | 13:04:17.913 | II | SwiftBAT | (64) | 4 | S2 | 62.7 | 0.4791 | s | (122) |
GRB 130907A | 21:39:15.997 | 21:39:19.051 | II | SwiftBAT | (64) | 4 | S2 | 35.0 | 1.238 | s | (123) |
GRB 131030A | 20:56:17.811 | 20:56:13.932 | II | SwiftBAT | (64) | 4 | S1 | 90.9 | 1.293 | s | (124) |
GRB 131105A | 02:05:27.233 | 02:05:26.001 | II | SwiftBAT | (64) | 4 5 | S1 | 8.8 | 1.686 | s | (125) |
GRB 131108A | 20:41:52.947 | 20:41:55.851 | II | FermiLAT | (126) | 5 6 | S2 | 89.9 | 2.40 | s | (127) |
GRB 131231A | 04:45:32.361 | 04:45:31.276 | II | FermiLAT | (128) | 5 6 | S1 | 84.1 | 0.6439 | s | (129) |
GRB 140213A | 19:21:33.011 | 19:21:33.067 | II | SwiftBAT | (64) | 4 5 | S1 | 8.4 | 1.2076 | s | (130) |
GRB 140419A | 04:06:51.110 | 04:06:50.972 | II | SwiftBAT | (64) | 4 | S2 | 63.7 | 3.956 | s | (131) |
GRB 140506A | 21:07:39.098 | 21:07:37.801 | II | SwiftBAT | (64) | 4 5 | S1 | 57.8 | 0.889 | s | (132) |
GRB 140508A | 03:03:58.423 | 03:03:57.067 | II | SwiftBAT | (64) | 5 | S2 | 24.6 | 1.027 | s | (133) |
GRB 140512A | 19:31:50.769 | 19:31:49.555 | II | SwiftBAT | (64) | 4 5 | S2 | 82.9 | 0.725 | s | (134) |
GRB 140606B | 03:11:50.769 | 03:11:52.293 | II | SwiftBAT | (64) | 5 | S2 | 46.8 | 0.384 | s | (135) |
GRB 140801A | 18:59:54.769 | 18:59:54.138 | II | FermiGBM | (136) | 5 | S2 | 81.2 | 1.320 | s | (136) |
GRB 140808A | 00:53:59.264 | 00:54:01.038 | II | FermiGBM | (137) | 5 | S2 | 31.6 | 3.293 | s | (138) |
GRB 141220A | 06:02:51.666 | 06:02:52.662 | II | SwiftBAT | (64) | 4 5 | S2 | 54.8 | 1.3195 | s | (139) |
GRB 150206A | 14:31:20.265 | 14:31:22.868 | II | SwiftBAT | (64) | 4 | S1 | 31.8 | 2.087 | s | (140) |
GRB 150314A | 04:54:51.727 | 04:54:50.924 | II | SwiftBAT | (64) | 4 5 6 | S2 | 46.9 | 1.758 | s | (141) |
GRB 150323A | 02:51:22.369 | 02:51:20.908 | II | SwiftBAT | (64) | 4 | S2 | 64.3 | 0.593 | s | (142) |
GRB 150403A | 21:54:12.693 | 21:54:13.255 | II | SwiftBAT | (64) | 4 5 6 | S1 | 47.3 | 2.06 | s | (143) |
GRB 150424A | 07:43:01.073 | 07:42:57.738 | I | SwiftBAT | (64) | 4 | S1 | 54.8 | 0.30o | s | (144) |
GRB 150514A | 18:35:05.130 | 18:35:05.725 | II | FermiLAT | (145) | 5 6 | S1 | 8.7 | 0.807 | s | (146) |
GRB 150821A | 09:44:34.166 | 09:44:31.096 | II | SwiftBAT | (64) | 4 5 | S1 | 44.7 | 0.755 | s | (147) |
GRB 151021A | 01:28:56.535 | 01:28:52.888 | II | SwiftBAT | (64) | 4 | S1 | 67.9 | 2.330 | s | (148) |
GRB 151027A | 03:58:24.154 | 03:58:24.488 | II | SwiftBAT | (64) | 4 5 | S2 | 5.3 | 0.81 | s | (149) |
GRB 160131A | 08:20:44.577 | 08:20:43.817 | II | SwiftBAT | (64) | 4 | S1 | 60.1 | 0.972 | s | (150) |
GRB 160410A | 05:09:52.644 | 05:09:48.172 | Ip | SwiftBAT | (64) | 4 | S1 | 82.0 | 1.717 | s | (151) |
GRB 160509A | 08:58:46.696 | 08:58:48.075 | II | FermiLAT | (152) | 5 6 | S2 | 15.8 | 1.17 | s | (153) |
GRB 160623A | 04:59:37.594 | 04:59:36.336 | II | FermiLAT | (154) | 5 6 | S2 | 34.5 | 0.367 | s | (155) |
GRB 160625B | 22:40:19.875 | 22:40:18.938 | II | FermiLAT | (156) | 4 5 6 | S2 | 65.1 | 1.406 | s | (157) |
GRB 160629A | 22:19:45.314 | 22:19:46.474 | II | INTEGRAL | (158) | 5 | S2 | 27.6 | 3.332 | s | (159) |
Notes.
a"Dark" burst according to the classification presented in the redshift reference paper. b"Dark" burst according to Fynbo et al. (2009). cPrompt emission observation(s): 1, CGRO-BATSE; 2, HETE-2; 3, BeppoSAX-GRBM; 4, Swift-BAT; 5, 6, Fermi-LAT. dRedshift types are s, spectroscopic and p, photometric. eAlthough this burst is referred to as GRB 020819 in all related GCN circulars and in some other publications, this is the second GRB observed by KW on 2002 August 19. fThis burst was initially referred to as GRB 050820, but, after the detection of GRB 050820B on the same day, it was renamed to GRB 050820A. gThe redshift at 95% confidence level is . hAlthough GRB 060121 is a short-duration burst, it was classified as the Type II (see, e.g., Zhang et al. 2009 or S16 for details). iThe redshift study of GRB 060121 (de Ugarte Postigo et al. 2006) revealed two probability peaks. The main one (with a 63% likelihood) places the burst at . A secondary peak (with a 35% likelihood) would imply that the afterglow lies at a . jThe type of GRB 060614 is uncertain: an SN-less, long-duration burst (Della Valle et al. 2006; Gal-Yam et al. 2006; Gehrels et al. 2006; Fynbo et al. 2006) is suggested to be a Type I burst based on its host galaxy low specific star-forming rate (Zhang et al. 2009), while in the KW data this GRB was classified as a Type II burst based on duration and hardness only (see S16 for details). kThis burst is a short burst with extended emission (EE) according to Sakamoto et al. (2011a) and S16. lThe 95% confidence redshift range is . mThe redshift at the confidence level is . nA rather wide 95% confidence range is reported for this estimate. oSince there is an ambiguity with the host galaxy identification, this redshift may not correspond to the burst. See the text (Section 3) for details. pAlthough this GRB cannot be unambiguously assigned into the Type I population, we classify it as Type I. See the text (Section 3) for details.References. (1) Frontera et al. (2009), (2) Bloom et al. (2001a), (3) Remillard et al. (1997), (4) Djorgovski et al. (2001), (5) Kulkarni et al. (1998), (6) Kulkarni et al. (1999), (7) Bloom et al. (2003a), (8) Vreeswijk et al. (2001), (9) Le Floch et al. (2002), (10) Hurley (1999), (11) Djorgovski et al. (1999), (12) Vreeswijk et al. (2006), (13) Kippen (2000), (14) Andersen et al. (2000), (15) Piro et al. (2002), (16) Smith et al. (2000), (17) Castro et al. (2000a), (18) Hurley et al. (2000a), (19) Hurley et al. (2000b), (20) Price et al. (2002a), (21) Hurley et al. (2000c), (22) Castro et al. (2000b), (23) Castro et al. (2001), (24) Price et al. (2002b), (25) Infante et al. (2001), (26) Masetti et al. (2002), (27) Table of HETE Burst Data (2006), (28) Barth et al. (2003), (29) Levesque et al. (2010), (30) Crew et al. (2002), (31) Della Valle et al. (2003), (32) Bloom et al. (2003b), (33) Fenimore et al. (2004), (34) Wiersema et al. (2004), (35) Galassi et al. (2004), (36) Price et al. (2004), (37) Sakamoto et al. (2011a), (38) Watson et al. (2006), (39) Foley et al. (2005), (40) Berger & Becker (2005), (41) Fox et al. (2008), (42) Jakobsson et al. (2006), (43) Volnova et al. (2014), (44) Gal-Yam et al. (2005), (45) Quimby et al. (2005), (46) Soderberg et al. (2006), (47) Prigozhin et al. (2006), (48) de Ugarte Postigo et al. (2006), (49) Fynbo et al. (2009), (50) Della Valle et al. (2006), (51) Krühler et al. (2012), (52) Levan et al. (2007), (53) Berger et al. (2007a), (54) Krühler et al. (2015), (55) Stratta et al. (2007), (56) Perley et al. (2009), (57) Hurley & Cline (2007), (58) Cenko et al. (2008), (59) Jakobsson et al. (2007), (60) Perley et al. (2013), (61) Graham et al. (2009), (62) Perley et al. (2008), (63) Stern et al. (2007), (64) Swift GRB Table (2016), (65) Berger et al. (2007b), (66) Rapisarda et al. (2008), (67) Rossi et al. (2008), (68) Prochaska et al. (2009), (69) Starling et al. (2009), (70) Fermi-LAT Collaboration (2013), (71) Greiner et al. (2009), (72) Berger & Rauch (2008), (73) Kuin et al. (2009), (74) Salvaterra et al. (2012), (75) Cucchiara et al. (2008), (76) de Ugarte Postigo et al. (2009b), (77) Chornock et al. (2009a), (78) Cenko et al. (2009a), (79) Chornock et al. (2009b), (80) Rau et al. (2009), (81) Cenko et al. (2009b), (82) Wiersema et al. (2009), (83) de Ugarte Postigo et al. (2009a), (84) Malesani et al. (2009), (85) Cucchiara et al. (2009), (86) Xu et al. (2009), (87) Sakamoto et al. (2009), (88) Chornock & Berger (2009), (89) Thoene et al. (2009), (90) Cenko et al. (2010), (91) Cucchiara & Fox (2010), (92) Milvang-Jensen et al. (2010), (93) Kruehler et al. (2013), (94) O'Meara et al. (2010), (95) Tanvir et al. (2010b), (96) Tanvir et al. (2010c), (97) Chornock & Berger (2011a), (98) Chornock & Berger (2011b), (99) Milne & Cenko (2011), (100) de Ugarte Postigo et al. (2011a), (101) de Ugarte Postigo et al. (2011b), (102) Piranomonte et al. (2011), (103) Tanvir et al. (2011), (104) Hurley et al. (2011), (105) de Ugarte Postigo et al. (2011c), (106) Sparre et al. (2014), (107) Palazzi et al. (2011), (108) Cucchiara & Prochaska (2012), (109) de Ugarte Postigo et al. (2013a), (110) IBAS: Results (2012), (111) Tanvir et al. (2012b), (112) Hurley et al. (2012), (113) D'Elia et al. (2012), (114) Berger et al. (2013), (115) Tanvir et al. (2012a), (116) Hjorth et al. (2013), (117) Flores et al. (2013), (118) Tanvir et al. (2013), (119) Cucchiara & Cenko (2013), (120) de Ugarte Postigo et al. (2014c), (121) Xu et al. (2013a), (122) Cucchiara & Perley (2013), (123) de Ugarte Postigo et al. (2013c), (124) Xu et al. (2013b), (125) Xu et al. (2013c), (126) Racusin et al. (2013), (127) de Ugarte Postigo et al. (2013b), (128) Sonbas et al. (2013), (129) Cucchiara (2014), (130) Schulze et al. (2014), (131) Tanvir et al. (2014), (132) Fynbo et al. (2014), (133) Wiersema et al. (2014), (134) de Ugarte Postigo et al. (2014a), (135) Perley et al. (2014), (136) Lipunov et al. (2016), (137) FERMIGBRST—Fermi-GBM Burst Catalog (von Kienlin et al. 2014; Gruber et al. 2014; Narayana Bhat et al. 2016), (138) Singer et al. (2015), (139) de Ugarte Postigo et al. (2014b), (140) Kruehler et al. (2015), (141) de Ugarte Postigo et al. (2015a), (142) Perley & Cenko (2015), (143) Pugliese et al. (2015), (144) Castro-Tirado et al. (2015), (145) Kocevski & Arimoto (2015), (146) de Ugarte Postigo et al. (2015c), (147) D'Elia et al. (2015), (148) de Ugarte Postigo et al. (2015b), (149) Perley et al. (2015), (150) de Ugarte Postigo et al. (2016), (151) Selsing et al. (2016), (152) Longo et al. (2016), (153) Tanvir et al. (2016), (154) Vianello et al. (2016), (155) Malesani et al. (2016), (156) Dirirsa et al. (2016), (157) Xu et al. (2016), (158) Gotz et al. (2016), (159) Castro-Tirado et al. (2016).
A machine-readable version of the table is available.
The "Type" column specifies the burst "physical" classification: Type I, the merger origin (Blinnikov et al. 1984; Paczynski 1986; Eichler et al. 1989; Paczynski 1991; Narayan et al. 1992), typically short/hard bursts, and Type II, the collapsar origin (Woosley 1993; Paczyński 1998; MacFadyen & Woosley 1999; Woosley & Bloom 2006), typically long/soft GRBs; see, e.g., Zhang et al. (2009) for more information on this classification scheme. According to the KW Type I/II criteria (S16), 11 GRBs from the sample can be confidently classified as Type I and 137 GRBs as Type II. Although for GRB 160410A exceeds 0.6 s, a threshold used by S16 to distinguish between "short" and "long" KW GRBs, this burst may be classified as Type I based on its position in the hardness–duration distribution of a large sample of KW bright GRBs (Figure 1), and also on its short (see Section 4.1 for definitions of T50 and T90). The physical classification of GRB 060614 is unclear: an SN-less, long-duration burst (Della Valle et al. 2006; Fynbo et al. 2006; Gal-Yam et al. 2006; Gehrels et al. 2006) was suggested to be Type I based on a low specific star-forming rate of its host galaxy (Zhang et al. 2009); conversely, from the KW prompt-emission analysis this GRB was classified by S16 as Type II, that we will use in this paper. Thus, of 150 GRBs in the sample, we designate 138 GRBs as Type II and 12 (or 8% of the sample) as Type I.
The next column indicates the mission/instrument that provided the most accurate GRB localization from prompt emission observations, thus enabling further identification of the source. Among 150 bursts in this catalog, 103 (or ∼2/3) are Swift-BAT GRBs, 13 were localized by BeppoSAX, 14 by Fermi (LAT and/or GBM), 8 by HETE-2, 2 by INTEGRAL-IBIS/ISGRI, and 2 by RXTE-ASM; for 10 GRBs, the best "prompt" localization was obtained with the help of triangulation by the IPN (Hurley et al. EAS Pub Ser., 61, 459, 2013). The "Other obs." column provides the information on the burst prompt emission detections by other missions with spectrometric capabilities in hard X-ray and γ-ray domains. The statistics of these detections are as follows: CGRO-BATSE—5, HETE-2—10, BeppoSAX-GRBM—13, Swift-BAT—102, Fermi-GBM—52, and Fermi-LAT—21. The "Det." and "Inc. angle" columns specify the KW triggered detector and the angle between the GRB direction and the detector axis (the incident angle).
The rightmost three columns of Table 1 contain the redshift data. For a number of GRBs there are several independent redshift estimates available, of which we gave a preference to spectroscopic over photometric redshifts, if available; also, results from refereed papers, which presented a detailed spectral analysis, were given higher priority over earlier GCN circulars. The redshift study of GRB 060121 (de Ugarte Postigo et al. 2006) revealed two probability peaks. The main one (which we chose for this catalog, with a 63% likelihood) places the burst at . A secondary peak (with a 35% likelihood) would imply that the source lies at . The redshift estimate we use for GRB 150424A (, Castro-Tirado et al. 2015) is based on the observation of a galaxy 5'' (22.5 kpc at this z) away from the afterglow position reported by Perley & McConnell (2015). We note, however, that Tanvir et al. (2015) found a fainter potential host galaxy with a likely redshift of underlying the GRB position.
Figure 2 shows KW GRB redshift distributions along with those for the pre-Swift-era GRBs and all GRB redshifts measured to mid-2016. The KW GRB redshifts span the range and have mean and median values of ∼1.5 and ∼1.3, respectively. These statistics are comparable with those for the pre-Swift era GRBs, whose distribution peaks at (Berger et al. 2005), but they are significantly lower than the Swift-era values (; Coward et al. 2013). The fraction of the KW-detected GRBs is ∼0.4–0.5 at and it gradually decreases with z; for short/hard (Type I) bursts the fraction is ∼0.5. The absence of high-redshift bursts () in the KW sample results from several instrument-specific biases discussed further in this paper.
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Standard image High-resolution image4. Data Analysis and Results
4.1. Burst Durations and Spectral Lags
4.1.1. Analysis
The total burst duration T100, and the T90 and T50 durations (the time intervals that contain 5% to 95% and 25% to 75% of the total burst count fluence, respectively; see, e.g., Kouveliotou et al. 1993), were determined, in this work, using the counts in G2+G3 energy band (∼80–1200 keV at present). The soft energy band G1 was excluded from the analysis for a number of reasons, i.e., (1) the major fraction of the GRB spectra have the peak energy of the spectrum and hence photons responsible for the burst energy are detected mostly in the G2 and G3 bands; (2) the KW background in G2 and G3 is very stable (in contrast to background in the soft energy range G1 (∼20–80 keV), which can exhibit significant variations due to solar activity and hard X-ray transients); (3) for some bursts, an emerging X-ray afterglow may be confused with the prompt emission in G1.
To compute the durations, a concatenation of waiting-mode and triggered-mode light curves was used. The burst's start and end times were determined at 5σ excess above background on timescales from 2 ms to 2.944 s in the interval from to (the end of the KW triggered mode record). In some cases, e.g., for GRB 020813, which partly overlaps in time with a solar flare, the search interval was narrowed to exclude the non-GRB event. The background was approximated by a constant, using, typically, the interval from to .
The spectral lag () is a quantitative measure of spectral evolution often seen in long GRBs, when the emission in a soft detector band peaks later or has a longer decay relative to a hard band; a positive corresponds to the delay of the softer emission. To derive spectral lags we used a cross-correlation method similar to that described in Band (1997) and Norris et al. (2000). The cross-correlation function (CCF) was computed between three pairs of KW energy channels: G2–G1, G3–G1, and G2–G3. For each pair of channels (Gi,Gj) the peak of fourth-degree polynomial fit for the CCF was taken as . The error was estimated via the bootstrap approach. To ensure the robustness of the analysis, only bursts featuring a single emission episode, with start and end times being within the triggered mode record, were selected for the spectral lag calculations.
4.1.2. Results
Table 2 summarizes the results of our temporal and lag analyses. The first column contains the GRB name (see Table 1). Next, the values of T100, T90, and T50 are listed along with the corresponding start times t0, t5, and t25 given relative to the trigger time T0. For GRB 081203A, which was detected during the data output of GRB 081203B, no high-resolution light curves are available and, thus, only a rough estimate of T100 is provided. While for weak KW GRBs, T100 and T90 are nearly similar measures of duration (Figure 3), for brighter bursts, T100 becomes more sensitive to the existence of weak precursors or extended tails. This behavior is particularly apparent for such remarkable events as the "naked-eye" GRB 080319B (Racusin et al. 2008); the ultra-luminous GRB 110918A (Frederiks et al. 2013); the nearby, ultra-bright GRB 130427A (Maselli et al. 2014); and two recent highly energetic events, GRB 160623A (Frederiks et al. 2016) and GRB 160625B (Svinkin et al. 2016a; Zhang et al. 2016). The latter burst features a precursor separated from the main episode by a long interval of quiescence and the four former bursts are characterized by slowly decaying tails of hard X-ray emission that were bright enough to be detected in the KW G2 band for hundreds of seconds.
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Standard image High-resolution imageTable 2. Durations and Spectral Lags
Burst | t0 | T100 | t5 | T90 | t25 | T50 | |||
---|---|---|---|---|---|---|---|---|---|
Name | (s) | (s) | (s) | (s) | (s) | (s) | (s) | (s) | (s) |
GRB 970228 | −0.456 | 56.584 | −0.002 ± 0.024 | 53.442 ± 2.891 | 0.592 ± 0.048 | 39.280 ± 2.556 | ⋯ | ⋯ | ⋯ |
GRB 970828 | −4.248 | 94.936 | 0.864 ± 0.112 | 66.208 ± 2.781 | 7.680 ± 0.161 | 17.792 ± 0.310 | ⋯ | ⋯ | ⋯ |
GRB 971214 | −9.060 | 16.564 | −9.060 ± 2.082 | 15.892 ± 2.133 | −3.172 ± 2.951 | 6.724 ± 2.970 | ⋯ | ⋯ | ⋯ |
GRB 990123 | −17.312 | 111.200 | 1.600 ± 0.161 | 62.016 ± 1.179 | 7.904 ± 0.072 | 26.336 ± 0.757 | 0.681 ± 0.091 | 0.619 ± 0.099 | 0.165 ± 0.050 |
GRB 990506 | −0.390 | 164.742 | 1.952 ± 0.041 | 128.608 ± 0.654 | 12.032 ± 0.088 | 83.392 ± 2.565 | ⋯ | ⋯ | ⋯ |
GRB 990510 | −0.320 | 69.568 | 0.688 ± 0.186 | 55.888 ± 8.108 | 38.976 ± 1.735 | 5.760 ± 1.745 | ⋯ | ⋯ | ⋯ |
GRB 990705 | −1.698 | 67.746 | 1.648 ± 0.066 | 33.232 ± 1.120 | 7.488 ± 0.096 | 14.720 ± 0.211 | 0.053 ± 0.016 | 0.103 ± 0.063 | 0.016 ± 0.014 |
GRB 990712 | −1.637 | 18.821 | −1.637 ± 0.862 | 16.629 ± 1.777 | 0.784 ± 0.173 | 10.784 ± 0.470 | ⋯ | ⋯ | ⋯ |
GRB 991208 | −0.148 | 76.436 | 0.688 ± 0.016 | 63.056 ± 0.481 | 5.136 ± 1.562 | 53.680 ± 1.567 | ⋯ | ⋯ | ⋯ |
GRB 991216 | −17.477 | 44.629 | 0.672 ± 0.032 | 14.528 ± 0.140 | 3.264 ± 0.025 | 4.704 ± 0.154 | ⋯ | ⋯ | ⋯ |
GRB 000131 | −77.719 | 105.735 | −74.775 ± 2.944 | 96.471 ± 3.125 | −18.839 ± 12.138 | 27.719 ± 12.280 | ⋯ | ⋯ | ⋯ |
Note. A positive value of the spectral lag corresponds to a delay of the soft photons.
Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.
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The last three columns of Table 2 present the spectral lags , , and . For the 58 GRBs selected for the spectral lag analysis, the numbers of lags calculated are as follows: (G2–G1)—55, (G3–G1)—32, and (G3–G2)—38. The missing lag values are not constrained; this may be due to a weak detection in one or both analyzed channels, or to a significant difference in a pulse shape between them.
Figure 4 presents the T50, T90, and T100 observer- and rest-frame distributions. The rest-frame quantities are the corresponding observer-frame values scaled by the time dilation factor 1/().We note that the observer-frame energy band G2+G3, in which the durations are calculated, corresponds to multiple energy bands in the source-frame thus introducing a variable energy-dependant factor which must be accounted for when analyzing the rest-frame durations. The same considerations apply to the spectral lags.
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Standard image High-resolution image4.2. Energy Spectra
4.2.1. Analysis
For each burst from our sample, two time intervals were selected for spectral analysis: time-averaged fits were performed over the interval closest to T100 (hereafter the TI spectrum); the peak spectrum corresponds to the time when the peak count rate (PCR) is reached. The peak spectrum accumulation time may vary from burst to burst depending on the GRB intensity and the presence of significant spectral evolution. For 38 bursts with poor count statistics, the TI and the peak spectra are measured over the same interval.
More than a dozen bursts from the sample show two or more emission episodes separated by periods of quiescence. In the majority of cases, all emission episodes were included to the TI spectrum. KW triggered on weak precursors of GRB 120716A and GRB 160625B. To maintain a reasonable signal-to-noise ratio, only the main episodes of these bursts contributed to the spectral analysis presented in this paper.
The spectral analysis was performed using XSPEC version 12.9.0 (Arnaud 1996). The raw count rate spectra were rebinned to have a minimum of 20 counts per channel to ensure Gaussian-distributed count statistics and fitted using the statistic. Each spectrum was fitted by two spectral models. The first model is the Band function (hereafter BAND; Band et al. 1993):
where α is the low-energy photon index and β is the high-energy photon index. The second spectral model is an exponentially cutoff power-law (CPL), parameterized as Ep:
In the only case where both "curved" models result in ill-constrained fits (GRB 080413B), a simple power-law (PL) function was used: . All the spectral models were normalized to the energy flux (F) in the 10 keV–10 MeV range (observer frame). The fits were performed in the energy range from ∼20 keV to the upper limit of 0.5–15 MeV, depending on the presence of statistically significant GRB emission in the MeV band and, also, on the stability of the background in the upper spectral channels, which are affected, for some GRBs, by solar particles. The parameter errors were estimated using the XSPEC command ERROR based on the change in fit statistic () which corresponds to the 68% CL.
For each spectrum, we present the results for the models whose parameters are constrained (hereafter, GOOD models). The best-fit spectral model (the BEST model) was chosen based on the difference in between the CPL and the BAND fits. The criterion for accepting a model with a single additional parameter is a change in of at least 6 (). This criterion is widely accepted for choosing between nested spectral models in GRB studies (see, e.g., Sakamoto et al. 2008; Krimm et al. 2009; Goldstein et al. 2012) and corresponds to an F test chance improvement probability of ∼0.015 for a reasonably good quality of fit (the reduced chi-squared, i.e., the chi-squared per degree of freedom (d.o.f.), ). It should be noted that in the KW GCN circulars a different approach is used for the best-fit model selection: BAND is preferred over CPL in the case of the constrained fit, and not dependent on .
4.2.2. Results
The 10 columns in Table 3 contain the following information: (1) the GRB name (see Table 1); (2) the spectrum type, where "i" indicates that the spectrum is TI, "p" means that the spectrum is peak; (3) and (4) contain the spectrum start time (relative to T0) and its accumulation time (5) GOOD models for each spectrum ( indicates the BEST model); (6)–(8) α, β, and (9) F (normalization); (10) along with the null hypothesis probability given in brackets. In cases where the lower limit for β is not constrained, the value of () is provided instead, where is the lower limit for the fits. For the best-fit values of , only the upper limits on β are given.
Table 3. Spectral Parameters
Burst | Spec. | Model | α | β | F | ||||
---|---|---|---|---|---|---|---|---|---|
Name | Type | (s) | (s) | (keV) | ( erg cm−2 s−1) | (Prob.) | |||
GRB 970228 | i | 0.000 | 8.448 | CPLa | ⋯ | 44.9/56 (0.86) | |||
i | Band | 44.5/55 (0.84) | |||||||
p | 0.000 | 0.256 | CPLa | ⋯ | 13.3/24 (0.96) | ||||
p | Band | 13.0/23 (0.95) | |||||||
GRB 970828 | i | 0.000 | 70.656 | CPL | ⋯ | 72.6/66 (0.27) | |||
i | Banda | 63.5/65 (0.53) | |||||||
p | 17.920 | 5.120 | CPL | ⋯ | 68.6/79 (0.79) | ||||
p | Banda | 57.6/78 (0.96) | |||||||
GRB 971214 | i | 0.000 | 8.448 | CPLa | ⋯ | 72.2/78 (0.66) | |||
i | Band | 67.8/77 (0.77) |
Note.
aIndicates the BEST model for the spectrum.Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.
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Although KW high-resolution spectra do not cover the pre-trigger emission, for about two-thirds of GRBs in our sample the TI spectra include of the burst counts (and only for six bursts this fraction is ). A major fraction of the GRB 090812 counts, about one-half of the short GRB 100206A counts, and a significant fraction of the short GRB 070714B counts were accumulated before the trigger. For these bursts, we performed the spectral analysis using both multichannel spectra and the three-channel spectra constructed from light-curve data. Together, these spectra cover the burst T100 interval.
Figure 5 shows the distributions of spectral parameters. The CPL model's α for both TI and peak spectra are distributed around . For the BAND model, α for the TI and peak spectra are distributed around ≈−1 and ≈−0.85, respectively. The high-energy photon indices β for the TI and peak spectra are distributed around ≈−2.5 and ≈−2.35, respectively. We found BAND to be the BEST model for 54 TI and 51 peak spectra. The remaining spectra (with the exception of GRB 080413B) were best fitted by CPL. Ep for the BEST model varies from to (GRB 090510). The TI spectrum () distributions for both spectral models peak around 250 keV, while the peak spectrum () distributions peak around 300 keV. The corresponding rest-frame peak energies, and , vary from to (GRB 090510).
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Standard image High-resolution image4.3. Burst Energetics
4.3.1. Fluences and Peak Fluxes
The energy fluences (S) and the peak energy fluxes () were derived using the 10 keV–10 MeV energy fluxes of the BEST models for TI and peak spectra, respectively (Section 4.2). Since the TI spectrum accumulation interval typically differs from the T100 interval, a correction that accounts for the emission outside the TI spectrum was introduced when calculating S. Three timescales were used when calculating : together with two commonly utilized ones (1024 and 64 ms), we introduce the "rest-frame 64 ms" scale ( ms); the latter were used to estimate the rest-frame peak luminosity . To obtain , the model energy flux of the peak spectrum was multiplied by the ratio of the PCR on the scale to the average count rate in the spectral accumulation interval. Typically, the corrections were made using counts in the G2+G3 light curve; the G1+G2, G2 only, and G1+G2+G3 combinations were also considered depending on the emission hardness and intensity.
4.3.2. k-correction and Rest-frame Energetics
The cosmological rest-frame energetics, the isotropic-equivalent energy release and the isotropic-equivalent peak luminosity , can be calculated, with the proper k-correction, as and where is the luminosity distance. The k-correction to the rest-frame (see, e.g., Bloom et al. 2001b or Kovács et al. 2011 for details) is formulated in terms of spectral model energy flux F as
where , MeV] is our flux calculation band in the observer frame, and [E1, E2] is the rest-frame "bolometric" energy band. For E1, we accept 1 keV and for E2, we calculate . The latter value is higher than the widely used rest-frame limit of 10 MeV, since the upper boundary of the KW energy range is rather high ( MeV) and choosing would narrow the energy band of our observations.
4.3.3. Collimation-corrected Energetics
Knowing , one can estimate the collimation-corrected energy released in gamma-rays and the collimation-corrected peak luminosity , where is the jet opening angle and is the collimation factor.
In the case of a CBM with constant number density n, hereafter HM, is given by Sari et al. (1999):
where is the radiative efficiency of the prompt phase, is the prompt emitted energy in units of 1052 erg, and is measured in days. For calculations, we adopted canonical values and n = 1 cm−3 (Frail et al. 2001).
In the case of a stellar-wind-like CBM with , hereafter WM, the jet opening angle according to Li & Chevalier (2003) is
where /( g cm−1) is the wind parameter, is the mass-loss rate due to the wind, and is the wind velocity; is typical for a Wolf–Rayet star. Following Ghirlanda et al. (2007), we assume for all bursts with WM neglecting the unknown uncertainty of this parameter.
In this work, we only consider jet breaks that were detected either in optical/IR afterglow light curves or in two spectral bands simultaneously (e.g., in X-ray and in radio). Among ∼60 jet breaks reported for KW GRBs in the literature, 32 meet this criterion (including two for Type I bursts, GRB 051221A and GRB 030603B), and 23 of those GRBs have reasonable constraints on the CBM density profile (14 HM and 9 WM).
4.3.4. Results
Table 4 summarizes observer-frame and non-collimated rest-frame energetics. The first two columns are the GRB name and z. The next seven columns present the observer-frame energetics: S; peak fluxes on the three timescales ( (1024 ms), (64 ms), and ( ms)), together with start times of the intervals when the PCR is reached (, , and ). The next two columns contain and the peak isotropic luminosity, , calculated from . The provided values may be adjusted to a different timescale (64 or 1024 ms) as:
Table 4. Burst Energetics
Burst Name | z | Sb | c | d | c | d | c | d | e | f | d | |
---|---|---|---|---|---|---|---|---|---|---|---|---|
GRB 970228 | 0.69 | −0.512a | 0.106 | 0.118 | 12.01 ± 0.93 | 9.6 ± 1.5 | 0.92 | 1.32 | ||||
GRB 970828 | 0.96 | 20.256 | 20.416 | 20.416 | 262.2 ± 9.1 | 30.9 ± 3.6 | 1.1 | 1.85 | ||||
GRB 971214 | 3.42 | 2.752 | 5.664 | −0.280 | 146.3 ± 6.1 | 78 ± 13 | 0.44 | 4.05 | ||||
GRB 990123 | 1.60 | 5.872 | 6.048 | 5.984 | 2133 ± 54 | 490 ± 29 | 3.1 | 5.04 | ||||
GRB 990506 | 1.31 | 87.040 | 90.048 | 87.360 | 1255 ± 43 | 134.2 ± 7.6 | 0.92 | 3.80 | ||||
GRB 990510 | 1.62 | 44.160 | 44.224 | 44.544 | 174.2 ± 8.1 | 81.0 ± 9.6 | 0.76 | 3.37 | ||||
GRB 990705 | 0.84 | 14.000 | 15.856 | 15.824 | 218.1 ± 7.7 | 30.7 ± 2.8 | 0.84 | 2.02 | ||||
GRB 990712 | 0.43 | 10.880 | 11.456 | 11.504 | 3.86 ± 0.28 | 1.20 ± 0.18 | 1.1 | 0.50 | ||||
GRB 991208 | 0.71 | 56.256 | 56.960 | 56.960 | 233.4 ± 4.6 | 53.2 ± 2.1 | 0.61 | 3.30 | ||||
GRB 991216 | 1.02 | 3.840 | 4.032 | 3.952 | 886 ± 11 | 510 ± 21 | 1.6 | 5.73 | ||||
GRB 000131 | 4.50 | 2.144 | 2.880 | 2.672 | 1817 ± 56 | 859 ± 60 | 0.67 | 8.48 |
Notes.
aSince the trigger mode light curve begins at , the corresponding peak energy flux may be underestimated due to the absence of high-res data before . bIn units of erg cm−2. cThe start time of the time interval when the peak count rate is reached, s. dIn units of erg cm−2 s−1. eIn units of 1051 erg. fIn units of 1051 erg s−1.Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.
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The rightmost columns provide two additional characteristics useful when the sample selection effects are considered: the bolometric energy flux corresponding to the GRB detection threshold, (Section 5.3); and , the GRB detection horizon described in Section 5.4.
In Figure 6, the distributions of S, , , and are shown. The most fluent burst in this catalog is GRB 130427A ( erg cm−2). The brightest burst based on the peak energy flux is GRB 110918A ( erg cm−2 s−1). The most energetic burst in terms of the isotropic energy is GRB 090323 ( erg). The most luminous burst contained in this catalog is GRB 110918A ( erg s−1).
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Standard image High-resolution imageTable 5 summarizes the collimation-corrected energetics for 32 bursts with "reliable" jet break times. The first column is the burst name. The next three columns specify , the CBM environment implied (HM or WM), and references to them. The next two columns contain the derived and the corresponding collimation factor, and the last two columns present Eγ and Lγ. For bursts with no reasonable constraint on the CBM profile the results are given for both HM and WM.
Table 5. Collimation-corrected Parameters
Burst | CBM | Referencesa | Collimation | ||||
---|---|---|---|---|---|---|---|
Name | (days) | (deg) | factor () | (1049 erg) | (1049 erg s−1) | ||
GRB 990123 | WM | (1) | 1.91 ± 0.19 | 0.55 ± 0.12 | 118.10 ± 24.10 | 27.16 ± 5.74 | |
GRB 990510 | HM | (1) | 4.21 ± 0.09 | 2.70 ± 0.11 | 47.07 ± 3.20 | 21.90 ± 0.95 | |
GRB 990705 | 1b | HMc | (2) | 4.23 ± 0.32 | 2.72 ± 0.42 | 59.31 ± 9.13 | 8.36 ± 1.26 |
WM | 3.07 ± 0.16 | 1.43 ± 0.15 | 31.28 ± 3.21 | 4.41 ± 0.41 | |||
GRB 990712 | HMc | (3) | 9.20 ± 0.42 | 12.90 ± 1.19 | 4.96 ± 0.68 | 1.54 ± 0.28 | |
WM | 10.10 ± 0.35 | 15.50 ± 1.09 | 5.98 ± 0.60 | 1.85 ± 0.34 | |||
GRB 991216 | WM | (1) | 2.16 ± 0.06 | 0.71 ± 0.04 | 63.13 ± 3.88 | 36.32 ± 2.68 | |
GRB 000301C | HM | (4) | 9.33 ± 0.30 | 13.20 ± 0.85 | 44.56 ± 7.20 | 74.95 ± 8.08 | |
GRB 000418 | HMc | (1) | 9.62 ± 1.25 | 14.10 ± 3.87 | 134.50 ± 44.78 | 53.39 ± 16.34 | |
WM | 6.09 ± 0.53 | 5.65 ± 1.03 | 54.04 ± 12.13 | 21.44 ± 4.70 | |||
GRB 000926 | WM | (1) | 3.07 ± 0.06 | 1.43 ± 0.06 | 39.83 ± 2.46 | 16.24 ± 2.05 | |
GRB 010222 | WM | (5), (1) | 1.88 ± 0.06 | 0.54 ± 0.03 | 57.63 ± 3.81 | 12.56 ± 1.17 | |
GRB 010921 | HM | (6) | 25.51 ± 1.37 | 97.50 ± 10.60 | 105.70 ± 16.10 | 16.98 ± 2.43 | |
GRB 011121 | WM | (1) | 4.49 ± 0.16 | 3.07 ± 0.23 | 30.39 ± 2.26 | 4.09 ± 0.42 | |
GRB 020405 | WM | (1) | 4.56 ± 0.21 | 3.16 ± 0.30 | 37.07 ± 3.65 | 5.45 ± 0.74 | |
GRB 020813 | HM | (1) | 3.04 ± 0.37 | 1.41 ± 0.36 | 106.70 ± 27.01 | 22.22 ± 5.49 | |
GRB 030329 | HM | (7) | 6.02 ± 0.23 | 5.51 ± 0.43 | 9.11 ± 0.87 | 1.23 ± 0.10 | |
GRB 041006 | WM | (1) | 5.13 ± 0.23 | 4.00 ± 0.37 | 2.75 ± 0.26 | 2.15 ± 0.42 | |
GRB 050401 | HMc | (8) | 3.38 ± 0.42 | 1.74 ± 0.46 | 80.59 ± 21.26 | 36.98 ± 10.05 | |
WM | 2.33 ± 0.20 | 0.83 ± 0.14 | 38.38 ± 6.78 | 17.61 ± 3.45 | |||
GRB 050525A | HMc | (9) | 2.83 ± 0.06 | 1.22 ± 0.05 | 3.43 ± 0.17 | 2.33 ± 0.10 | |
WM | 3.31 ± 0.05 | 1.67 ± 0.05 | 4.68 ± 0.16 | 3.18 ± 0.19 | |||
GRB 050820A | HM | (10) | 7.99 ± 0.33 | 9.70 ± 0.83 | 1005.00 ± 95.19 | 133.80 ± 12.13 | |
GRB 051221A | 5b | HM | (11) | 14.04 ± 1.06 | 29.90 ± 4.66 | 9.20 ± 1.51 | 67.56 ± 10.47 |
GRB 060614 | HM | (12) | 9.72 ± 0.11 | 14.30 ± 0.32 | 3.89 ± 0.31 | 0.42 ± 0.02 | |
GRB 061121 | 1.16b | HM | (13) | 3.94 ± 0.30 | 2.36 ± 0.37 | 71.67 ± 11.46 | 53.35 ± 8.32 |
GRB 070125 | 3.78b | HM | (14) | 4.94 ± 0.37 | 3.71 ± 0.58 | 474.00 ± 74.85 | 108.20 ± 16.58 |
GRB 071010B | HMc | (15) | 9.22 ± 0.41 | 12.90 ± 1.16 | 18.72 ± 2.71 | 8.55 ± 1.06 | |
WM | 8.12 ± 0.30 | 10.00 ± 0.74 | 14.50 ± 1.61 | 6.62 ± 1.22 | |||
GRB 080319B | WM | (16), (12) | 3.41 ± 0.07 | 1.77 ± 0.08 | 278.10 ± 12.20 | 21.00 ± 1.30 | |
GRB 090328 | HM | (17), (12) | 10.73 ± 4.13 | 17.50 ± 16.00 | 190.20 ± 149.00 | 59.56 ± 46.09 | |
GRB 090618 | HM | (18) | 3.42 ± 0.28 | 1.78 ± 0.31 | 45.04 ± 8.08 | 4.74 ± 0.79 | |
GRB 090926A | HM | (17), (12) | 6.20 ± 0.47 | 5.85 ± 0.91 | 1234.00 ± 188.70 | 549.80 ± 82.86 | |
GRB 091127 | HMc | (19) | 4.46 ± 0.09 | 3.02 ± 0.13 | 4.82 ± 0.63 | 3.45 ± 0.29 | |
WM | 4.92 ± 0.10 | 3.68 ± 0.15 | 5.87 ± 0.63 | 4.20 ± 0.74 | |||
GRB 110503A | HMc | (20) | 3.80 ± 0.19 | 2.20 ± 0.23 | 46.80 ± 5.07 | 42.85 ± 4.31 | |
WM | 2.87 ± 0.10 | 1.26 ± 0.09 | 26.71 ± 1.93 | 24.46 ± 2.28 | |||
GRB 130427A | HM | (21) | 2.91 ± 0.13 | 1.29 ± 0.12 | 114.80 ± 10.09 | 35.64 ± 3.11 | |
GRB 130603B | HMc | (22) | 6.43 ± 0.23 | 6.29 ± 0.46 | 1.23 ± 0.10 | 18.79 ± 1.37 | |
WM | 8.90 ± 0.24 | 12.00 ± 0.66 | 2.36 ± 0.13 | 36.00 ± 3.00 | |||
GRB 151027A | 2.3b | WM | (23) | 6.08 ± 0.36 | 5.63 ± 0.68 | 18.60 ± 2.74 | 4.41 ± 0.73 |
Notes.
aIn cases where two references are given, the first one corresponds to the estimate and the second one corresponds to the preferred CBM. bWhen no uncertainty is available from the literature, we take the sample-mean as a 68% error for the calculations. cIn cases where no preferred CBM density profile is available from the literature, we provide the estimates for both HM and WM.References. (1) Zeh et al. (2006), (2) Masetti et al. (2000), (3) Björnsson et al. (2001), (4) Berger et al. (2000), (5) Galama et al. (2003), (6) Price et al. (2003), (7) Resmi et al. (2005), (8) Ghirlanda et al. (2007), (9) Blustin et al. (2006), (10) Cenko et al. (2006), (11) Soderberg et al. (2006), (12) Schulze et al. (2011), (13) Page et al. (2007), (14) Chandra et al. (2008), (15) Kann et al. (2007), (16) Tanvir et al. (2010a), (17) Cenko et al. (2011), (18) Cano et al. (2011), (19) Filgas et al. (2011), (20) Kann et al. (2011), (21) Maselli et al. (2014), (22) Fong et al. (2014), (23) Nappo et al. (2017).
Only a portion of this table is shown here to demonstrate its form and content. A machine-readable version of the full table is available.
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Table 6. Parameter Statistics
Parameter | Min | Max | Mean | Median |
---|---|---|---|---|
Name | Value | Value | Value | Value |
Redshift | 0.096 | 5 | 1.50 | 1.32 |
T100 (s) | 0.124 | 484.858 | 67.689 | 37.312 |
T90 (s) | 0.070 | 440.826 | 46.557 | 21.664 |
T50 (s) | 0.034 | 167.290 | 16.959 | 7.616 |
(s) | 0.088 | 170.884 | 29.476 | 13.974 |
(s) | 0.052 | 121.954 | 19.447 | 9.677 |
(s) | 0.025 | 49.733 | 7.220 | 3.002 |
(ms) | 0.6 | 2495 | 292 | 150 |
(ms) | 4.8 | 5106 | 543 | 343 |
(ms) | 2.1 | 765 | 176 | 132 |
(ms) | 0.4 | 1290 | 143 | 68 |
(ms) | 3.7 | 2630 | 257 | 133 |
(ms) | 1.4 | 388 | 85 | 68 |
(keV), Type I GRBs | 468 | 3516 | 953 | 640 |
(keV) Type I GRBs | 468 | 3386 | 966 | 671 |
(keV) Type I GRBs | 658 | 6691 | 1637 | 988 |
(keV) Type I GRBs | 658 | 6444 | 1647 | 991 |
(keV) Type II GRBs | 37 | 1083 | 298 | 238 |
(keV) Type II GRBs | 37 | 1511 | 360 | 271 |
(keV) Type II GRBs | 54 | 2703 | 775 | 661 |
(keV) Type II GRBs | 53 | 5137 | 931 | 752 |
S (erg cm−2) | 1.13 × 10−6 | 2.86 × 10−3 | 1.07 × 10−4 | 2.51 × 10−5 |
Fpeak,1024 (erg cm−2 s−1) | 5.56 × 10−7 | 5.08 × 10−4 | 1.42 × 10−5 | 3.45 × 10−6 |
(erg cm−2 s−1) | 9.51 × 10−7 | 9.02 × 10−4 | 2.55 × 10−5 | 6.19 × 10−6 |
(erg cm−2 s−1) | 6.89 × 10−7 | 8.71 × 10−4 | 2.33 × 10−5 | 5.41 × 10−6 |
(erg) | 4.18 × 1049 | 5.81 × 1054 | 5.55 × 1053 | 1.93 × 1053 |
(erg s−1) | 2.94 × 1050 | 4.65 × 1054 | 2.55 × 1053 | 8.32 × 1052 |
Collimation factor | 5.4 × 10−4 | 3.0 × 10−2 | 6.5 × 10−3 | 3.2 × 10−3 |
(erg) | 1.70 × 1049 | 1.23 × 1052 | 1.04 × 1051 | 3.98 × 1050 |
(erg s−1) | 4.22 × 1048 | 5.50 × 1051 | 4.39 × 1050 | 1.62 × 1050 |
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The jet opening angles vary from 19 to 255 and the corresponding collimation factors from to 0.098. The brightest KW GRB in terms of both and is GRB 090926A ( erg, erg s−1, ). The distributions of and are shown in Figure 6 and Table 6 provides descriptive statistics of the GRB parameters estimated in Section 4.
5. Discussion
5.1. This Catalog versus Previously Reported KW Results
Preliminary results on the KW detections of bursts with known redshifts have been reported in more than 100 GCN circulars and the more detailed KW GRB analyses were presented in multiple refereed publications. Although the latter results are, with a few exceptions, statistically consistent with those reported here, the main advantage of this catalog, in comparison to the previous work, is in the use of the unified, systematic approach to re-analyse all 150 bursts in the sample. Particularly, GRB durations were calculated in the G2+G3 band that is less affected by the hard X-ray background variations; this also allows one to separate the hard GRB prompt emission from the emerging X-ray afterglow. The spectral analysis presented here gains an advantage from the most recent and accurate KW DRM; it also relies on a standard procedure for the TI spectrum interval selection based on T100. The burst energetics, S and are estimated, in this work, based on the BEST spectral models for TI and peak spectra, which also improves the flux calculation uncertainties. Finally, the reported rest-frame energetics rely on the k-correction procedure that utilizes the full spectral band of the instrument, and they are estimated using a common set of cosmology parameters. To summarize, the results presented in this catalog form a consistent set of observer- and rest-frame GRB parameters useful for further systematic studies.
5.2. Observer-frame Spectral Parameters
5.2.1. The Sample Statistics and Comparison of KW with BATSE and GBM Bursts
Although this catalog covers only a limited subset of the KW-detected GRBs (≈7.5% for the time span covered), a discussion of the derived spectral parameter distributions may be useful for the sample characterization.
Among 138 TI spectra of long (Type II) GRBs, 83 are best fit with the CPL model, 54 with the BAND function, and for one GRB both "curved" models failed. Similar fractions of the BEST models were obtained for the peak spectra: 86 CPL, 51 BAND, and one PL. We found the peak spectra to be harder, in terms of Ep, as compared to the TI spectra for >80% of the Type II GRBs, consistent with the well-known GRB hardness–intensity correlation (or "Golenetskii" relation; Golenetskii et al. 1983). Median values for the BEST model Ep are 297 keV and 357 keV for the TI and the peak spectra, respectively. The corresponding median α values are −1.00 and −0.87, and the median β values are −2.45 and −2.33.
The case where both "curved" models result in ill-constrained fits is the relatively weak GRB 080413B. For this burst, the KW PL slope is −2.00 ± 0.1 ( d.o.f.), suggesting a low Ep value. This PL slope is consistent with that derived with Swift-BAT/Suzaku-WAM joint fit (−1.92 ± 0.06; Krimm et al. 2009). The best spectral model for this GRB reported by Krimm et al. (2009) is the Band function with , , and (and this model is also compatible with the KW data, d.o.f.7 ), that yields erg. Thus, the KW erg derived for GRB 080413B from the PL fit is overestimated by a factor of ∼1.6 as compared to the more precise result of the joint BAT/WAM analysis.
Of 150 GRBs in the sample, 12 (or 8%) are classified as short/hard (Type I) bursts. This fraction is one-half that for all KW GRBs (S16), thus reflecting the complexity of their optical identifications and redshift measurements. All spectra of the Type I GRBs from this catalog are fitted best by the CPL function, with median α = −0.53 and median Ep = 640 keV. These results are consistent with the BEST model and the spectral parameter statistics for 293 KW short GRBs given in S16.
We compared the BEST spectral parameter statistics for the whole sample with those for the BATSE 5B (Goldstein et al. 2013) and Fermi-GBM (Gruber et al. 2014) catalogs. We found the KW mean and median parameter values, for both spectral models and for both TI and peak spectra, consistent, within 68% confidence intervals, with the statistics given in these catalogs. Meanwhile, we noticed some systematic differences between the instruments, e.g., the KW spectra are typically harder, in terms of Ep, than BATSE and GBM ones. The same is true when comparing the low-energy spectral indices: the KW α are, on average, shallower than those reported for BATSE and GBM. Finally, the typical KW β are shallower than the BATSE β, but they are steeper when compared to the typical GBM indices. These systematic differences may be explained by the different spectral ranges of the instruments: the KW upper spectral limit (∼10–15 MeV) is higher than that of BATSE (∼2 MeV), thus allowing for high Ep to be constrained better. In turn, the broad range of the GBM BGO detectors (up to ∼30 MeV) may result, for the BAND spectra, in better constrained β and, simultaneously, smaller Ep, when compared to the typical KW parameters. The KW-GBM spectral cross-calibration over a large sample of simultaneously observed GRBs is currently underway that will provide a more detailed analysis of the instrumental effects that could be affecting the scientific results from the GRB prompt emission data.
It also should be noted that the mean Ep for the KW sample is beyond the Swift-BAT energy range (15–150 keV), thus emphasizing the importance of the KW detections of Swift GRBs.
5.2.2. Spectral Indices
The difference between low- and high-energy photon indices, , may be helpful when investigating GRB emission processes in the framework of the synchrotron shock model (SSM) through comparing the observational and theoretical values of to constrain the synchrotron cooling regime and infer the electron power-law index (Preece et al. 2002). The distribution for TI and peak spectra fitted with the BAND model is shown in Figure 5 (panel c). The fact that no obvious peak in the distributions is seen may imply a diversity of electron power-law indices and/or different SSM cases at the burst sources. The median values of are 1.5 and 1.6 for the TI and the peak spectra, respectively. The peak spectrum distribution is slightly shifted toward the higher values in comparison with the TI spectrum one.
Additionally, we estimated the fraction of the bursts which violate the synchrotron "line-of-death" (see Preece et al. 1998 for details) and the synchrotron cooling limit. We found that the 68% confidence intervals (CIs) for the BEST model alpha lie completely above the synchrotron "line-of-death" for about 8% of the TI and 21% of the peak spectra; also, the 68% CIs lie completely below the synchrotron cooling limit for the 5% of the TI and 2% of the peak spectra.
5.3. Selection Effects
Selection effects are distortions or biases that usually occur when the observational sample is not representative of the true, underlying population. They play a crucial role for GRBs (Turpin et al. 2016; Dainotti & Del Vecchio 2017), which are particularly affected by the Malmquist bias effect that favors the brightest objects against faint objects at large distances, and these biases have to be taken into account when using GRBs as distance estimators, cosmological probes, and model discriminators.
For the sample of the KW triggered-mode GRBs with known redshifts, the selection effects fall into two categories: the KW-specific effects, caused by its trigger sensitivity to the burst prompt emission parameters; and the "external" biases arising in the process of localization and securing GRB redshifts, which are outside of the scope of this paper.
The KW triggered mode is activated when the count rate in the G2 window exceeds a threshold above the background on one of two fixed timescales , 1 s (applicable, with a few exceptions, to Type II bursts in our sample) or 140 ms (the Type I bursts). Thus, the burst's detection significance may be characterized by a PCR to background statistical uncertainty ratio (over the corresponding ). Although the KW trigger criterion cannot be easily translated into the GRB prompt emission characteristics (e.g., duration, rise-time, spectral shape, or energy flux), an investigation into how their combination may affect the trigger sensitivity to a specific burst may be done indirectly.
We estimated the energy flux sensitivity of the KW detectors following the methodology described in Band (2003). Figure 7 presents the limiting energy flux (10 keV–10 MeV) as a function of for s, for a burst incident angle , and the S1 detector calibration as of mid-2015. As can be seen, the energy flux threshold under these assumptions is erg cm−2 s−1 and there is a bias against the detection of soft-spectrum bursts with , especially with CPL spectra, due to the instrumental selection. Meanwhile, the F − Ep diagram stresses the lack of bright ( erg cm−2 s−1) and soft ( keV) GRBs, that should be easily detectable with KW. Since the lower boundary of this region is defined by GRBs with moderate-to-high detection significance, the instrumental biases do not affect the sample from this edge of the distribution. Thus, the apparent lack of soft/bright burst observations in the KW sample is likely due to an intrinsic GRB property (see Section 5.7 for more discussion).
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Standard image High-resolution imageIn a similar way, we calculated a limiting observer-frame energy flux for each GRB from the sample using its BEST-model spectral parameters, incident angle, and detector calibration. In order to make the results more helpful for the rest-frame energy calculations, we applied k-corrections (Section 4.3) to these values using the burst redshift. The resulting bolometric limiting fluxes, , are given in Table 4; the sample mean value of for the Type II GRBs is erg cm−2 s−1. We note that are calculated using the 1 s scale; when compared to peak fluxes determined on a different they should be adjusted as:
Figure 8 shows the KW GRB distributions in the –z, –z, and –z diagrams. The region in the –z plane above the limit corresponding to erg cm−2 s−1 may be considered free from the selection bias. In the –z plane, the selection-free region lies above the limit, corresponding to the bolometric fluence erg cm−2. As mentioned above, the KW detector sensitivity drops rapidly as Ep approaches the lower boundary of the instrument's band (∼20–25 keV as of 2015), and this results in a lack of bursts below in the –z plane; the additional factor here is due to cosmological time dilation.
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Standard image High-resolution imageFinally, our sample does not exhibit any direct selection effects due to GRB duration. However, some bursts with very gradual rising slopes may not trigger the instrument despite being bright enough to do it in other circumstances. We estimate the number of such GRBs with known redshifts to be (as of mid-2016); these bursts will be considered, along with other KW background-mode GRBs with known redshifts, in the second part of the catalog.
5.4. KW GRB Detection Horizon
Knowing the maximum distance at which a particular GRB can be detected by the instrument (the GRB "horizon," ) may be useful in a number of applications, e.g., for deriving the statistic (Schmidt et al. 1988) or for accounting for the instrumental bias when studying the "true" GRB energy distribution (Atteia et al. 2017).
A common approach to estimate the GRB horizon is to find a redshift , at which the limiting isotropic luminosity , defined by the limiting energy flux estimated for the whole sample (the "monolithic" ), starts to exceed the GRB . The KW trigger, however, is based on a simple photon-counting algorithm and not directly sensitive to the incident energy flux. Thus, the correctness of the described approach (hereafter the monolithic method), which doesn't account for the burst-specific instrumental issues, such as trigger sensitivity to the GRB incident angle, its light-curve shape, and the shape of the energy spectrum, needs an additional confirmation.
When evaluating how GRB detectability by KW changes when the burst source is shifted from its redshift z to a more distant , at least three effects have to be accounted for. First, the solid angle factor, which reduces (assuming identical beaming) an incident bolometric photon flux P by , where DM is the transverse comoving distance. Second, the cosmological time dilation, which results in the light curve broadening and an additional decrease in P by a factor of (1 + )/(1 + z). Finally, the spectral cutoff, which is inherent to GRB spectra, is redshifted by the same factor, thus decreasing the fraction of P within the instrument trigger band (G2). We estimate the KW detection horizon as a redshift , at which the PCR in the G2 light curve drops below the trigger threshold () on both KW trigger scales (140 ms and 1 s). is calculated as
where is the PCR reached in the observed G2 light curve on the modified timescale; is the BEST spectral model count flux in G2 calculated using the DRM; and is the corresponding flux in the redshifted spectrum. The resulting values of are given in Table 4 and shown in Figure 9. We found that for both Type I and Type II GRBs, are distributed narrowly around the corresponding values calculated assuming the bolometric erg cm−2 s−1 with the mean and σ of the distribution of 1.01 and 0.12, respectively. Although in some cases calculated with the simple monolithic method may differ from the more precisely evaluated by a factor of ∼1.5, our calculations support the general correctness of the former approach.
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Standard image High-resolution imageThe most distant GRB horizon for the KW sample () is reached for the ultra-luminous GRB 110918A8 at and the second-highest () is for GRB 050603 (). At , the age of the universe amounts to only ∼230 Myr, i.e., a burst that occurred close to the end of the cosmic Dark Ages could still trigger the KW detectors, and a thorough temporal and spectral analysis in a wide observer-frame energy range could be performed. Among the KW Type I GRBs, the highest is for GRB 160410A ().
5.5. GRB Luminosity and Isotropic-energy Functions, GRB Formation Rate
Among various statistical parameters, the luminosity function as well as the cosmic formation rate of GRBs are particularly interesting. The luminosity function (LF) is a measure of the number of bursts per unit luminosity, that provides information on the energy release and emission mechanism of GRBs. The cosmic GRB formation rate (GRBFR) is a measure of the number of events per comoving volume and time, which can help us to understand the production of GRBs at various stages of the universe. While LF was originally used to study long-lasting and relatively stable astrophysical phenomena, such as stars and galaxies, the isotropic energy release function (EF, the number of bursts per unit ) can be more representative for transient phenomena, e.g., for GRBs. The GRB EF was constructed for the first time by Wu et al. (2012) using a sample of 95 bursts with measured redshifts. The KW sample presented in this catalog provides an excellent opportunity to test GRB LF, EF, and GRBFR on an independent data set.
Without loss of generality, the total LF 9 can be rewritten as where is the GRB formation rate (GRBFR), is the local LF, is the luminosity evolution that parameterizes the correlation between L and z, and is the shape of the LF, whose effect is commonly ignored as the shape of the LF does not change significantly with z (e.g., Yonetoku et al. 2004). Following Lloyd-Ronning et al. (2002), Yonetoku et al. (2004), Wu et al. (2012), and Yu et al. (2015) we chose the functional form of for the luminosity evolution. It should be noted that the isotropic luminosity evolution can be determined by either the evolution of the amount of energy per unit time emitted by the GRB progenitor or by the jet opening angle evolution (see, e.g., Lloyd-Ronning et al. (2002) for the discussion); we tested the KW sample for a correlation between the collimation factor and z and found the correlation negligible (the Spearman rank-order correlation coefficient (the corresponding p value ) for the subsample of 30 Type II bursts with known collimation factors).
The KW z– and z– samples suffer from selection effects due to the detection limit of the instrument (see Section 5.3 for details) that results in data truncation seen in Figure 8. To estimate LF, EF, and GRBFR for the sample of 137 KW Type II bursts we used the non-parametric Lynden-Bell technique (Lynden-Bell 1971) further advanced by Efron & Petrosian (1992) (the EP method); the details of our calculations are described in the Appendix. The EP method is specifically designed to reconstruct the intrinsic distributions from the observed distributions, which accounts for the data truncations introduced by observational bias and includes the effects of the possible correlation between the two variables.
Applying the EP technique based on the individual (i.e., calculated for each burst independently) truncation limits to the z– plane, we found that the independence of the variables is rejected at (where τ is a modified version of the Kendall statistic, see the Appendix), and the best luminosity evolution index is ( CL). Similar results were obtained using the "monolithic" truncation limit erg cm−2 s−1: and .
Applying the same method to the z– plane and using the monolithic truncating fluence erg cm−2 (see the Appendix for the details of and selection), we found that the independence of the variables is rejected at , and the best isotropic energy evolution index is . Thus, the estimated and evolutions are comparable. The evolution PL indices and derived here are shallower than those reported in the previous studies: (Yonetoku et al. 2004), (Wu et al. 2012), (Yu et al. 2015), and (Wu et al. 2012), albeit within errors.
After eliminating the luminosity and energy release evolution, we, following Lynden-Bell (1971), obtained the local cumulative LF and EF, and , where and . We approximated the variance of and by bootstrapping the initial sample and fitted the distributions with a broken power-law (BPL) function:
where and are the PL indices at the dim and bright distribution segments and xb is the breakpoint of the distribution, and with the CPL function10 : , where is the cutoff luminosity (or energy).
The fits were performed in space using minimization, the results are given in Table 7 and shown in Figure 10 (right panel). The derived BPL slopes of LF and EF are close to each other, both for the dim and bright segments, thus the shape of EF is similar to that of LF; also, these indices are roughly consistent with the LF and EF slopes obtained in Yonetoku et al. (2004) and Wu et al. (2012). The small reduced obtained for both models do not allow us to reject any of them; however, when compared to BPL, the CPL fit to results in a considerably worse quality (); with the PL slope and the cutoff luminosity erg s−1. Conversely, the cutoff PL fits better when compared to BPL (); with and the cutoff energy erg. The existence of a sharp cutoff of the isotropic energy distribution distribution of KW and Fermi-GBM GRBs around erg was suggested recently by Atteia et al. (2017).
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Standard image High-resolution imageTable 7. LF and EF Fits with BPL and Cutoff PL
Data | Evolution | Model | xb,52 | |||
---|---|---|---|---|---|---|
(PL Index) | ( ) | |||||
BPL | 2.05 (133) | −0.47 ± 0.06 | −1.05 ± 0.11 | 0.27 ± 0.12 | ||
CPL | 18.5 (134) | −0.60 ± 0.04 | ⋯ | 2.10 ± 0.15 | ||
BPL | 19.2 (126) | −0.36 ± 0.01 | −1.28 ± 0.11 | 1.30 ± 0.04 | ||
CPL | 12.7 (127) | −0.31 ± 0.02 | ⋯ | 2.09 ± 0.04 | ||
no evolution | BPL | 2.32 (133) | −0.48 ± 0.06 | −1.00 ± 0.10 | 0.96 ± 0.15 | |
no evolution | CPL | 8.90 (134) | −0.54 ± 0.04 | ⋯ | 2.58 ± 0.11 | |
no evolution | BPL | 17.2 (126) | −0.35 ± 0.01 | −1.29 ± 0.12 | 1.80 ± 0.05 | |
no evolution | CPL | 15.4 (127) | −0.32 ± 0.01 | ⋯ | 2.63 ± 0.04 |
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The derived and correspond to the present-time GRB luminosity and energy distributions (at z = 0) and hence the local LF and EF in the comoving frame are roughly estimated as and , correspondingly. Taking into account that the z– and z– evolutions are established at , the LF and EF calculated without accounting for the evolution, and , may be of interest. We estimated these functions by setting and to zero, and found them very similar in shape to the present-time LF and EF (Figure 10). The results of the BPL and CPL fits to and are given in the last four lines of Table 7.
Finally, using the EP method, we estimated the cumulative GRB number distribution and the derived GRBFR per unit time per unit comoving volume (see the Appendix for the details). In Figure 11, we compare the star formation rate (SFR) data from the literature (Hopkins 2004; Hanish et al. 2006; Thompson et al. 2006; Li 2008; Bouwens et al. 2011) with GRBFRs derived from different z–L and z–E distributions. The GRBFR estimated from the evolution-corrected z– distribution exceeds the SFR at and nearly traces the SFR at higher redshifts; the same behavior is noted for the GRBFRs estimated using both the evolution-corrected z– and the non-corrected z– distributions. The low-z GRBFR excess over SFR is in agreement with the results reported in Yu et al. (2015) and Petrosian et al. (2015). Meanwhile, the only GRBFR that traces the SFR in the whole KW GRB redshift range is the derived from the z– distribution (i.e., not accounting for the luminosity evolution). Such behavior is known, e.g., from Wu et al. (2012), albeit for the GRBFR estimated from the z– distribution.
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Standard image High-resolution image5.6. Hardness-duration Distribution in the Observer and Rest Frames
Figure 12 shows as a function of the burst durations T90 in the observer and rest frames. In the observer frame the KW Type I GRBs are typically harder and shorter than Type II bursts, which is consistent with the classification obtained from the hardness–duration distribution (Figure 1), and this tendency shows no dependence on the burst redshift.
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Standard image High-resolution imageIn the cosmological rest frame, this pattern remains practically unchanged for GRBs at but it appears to be less distinct when the whole sample is considered. Although in the rest frame Type I GRBs are still shorter than Type II GRBs, their rest-frame Ep, clustered around 1 MeV, are superseded by those of a significant fraction of the Type II population. The notable exceptions here are GRB 090510 and GRB 160410A, whose rest-frame peak energies exceed those of even the highest-z Type II GRBs. We note, however, that the derived rest-frame durations are affected by a variable energy-dependant factor (Section 4.1) and the KW rest-frame Ep are subject to the observational bias (Section 5.3) thus an interpretation of the rest-frame hardness–duration distribution should be done with care.
5.7. Hardness–Intensity Correlations
Using the data described in the previous sections, we tested KW GRB characteristics against –S and – correlations in the observer frame, and – ("Amati") and – ("Yonetoku") correlations in the rest frame, along with their collimated versions –Eγ and –Lγ.
To probe the existence of correlations, we calculated the Spearman rank-order correlation coefficients () and the associated null-hypothesis (chance) probabilities or p values ( Press et al. 1992). The null hypothesis is that no correlation exists; therefore, a small p value indicates a significant correlation. It was shown that the Nukers' estimate is an unbiased slope estimator for the linear regression (Tremaine et al. 2002). The Nukers' estimate is based on minimizing:
where and are the measurement errors; thus both variables are treated symmetrically in terms of their errors and there is no need to choose dependent and independent variables. Although a correlation may be highly significant, the reduced statistic, , may be indicating that either the uncertainties are underestimated or there is an intrinsic dispersion in the correlation. To account for the intrinsic dispersion, an additional term, , is added to the denominator and, in this case, is adjusted to ensure . Therefore, we approximated a linear regression between -energy and Ep using two methods, without and with the intrinsic scatter.
Table 8 summarizes the correlation parameters we obtained for subsamples of Type I GRBs, Type II GRBs, and Type II GRBs with estimates. The first column presents the correlation. The next three columns provide the number of bursts in the fit sample, , and . The next columns specify the slopes (a), the intercepts (b), and . Since zeroing the intrinsic scatter yields for all the subsamples (and that confirms the relevance of accounting for ), their values are of little interest and we do not present the fit statistics in the table.
Table 8. Hardness–Intensity Correlations
Correlation | N | a | b | |||||
---|---|---|---|---|---|---|---|---|
Type I GRBs | ||||||||
versus S | 12 | 0.74 | 5.8 × 10−3 | 0.408 ± 0.043 | 4.98 ± 0.22 | 0.496 ± 0.117 | 5.52 ± 0.62 | 0.135 |
versus | 12 | 0.83 | 9.5 × 10−4 | 0.364 ± 0.030 | −15.70 ± 1.53 | 0.266 ± 0.068 | −10.61 ± 3.47 | 0.181 |
versus | 12 | 0.54 | 7.1 × 10−2 | 0.340 ± 0.045 | 4.39 ± 0.19 | 0.349 ± 0.161 | 4.52 ± 0.74 | 0.188 |
versus | 12 | 0.67 | 1.7 × 10−2 | 0.396 ± 0.034 | −17.68 ± 1.78 | 0.243 ± 0.078 | −9.61 ± 4.07 | 0.200 |
Type II GRBs | ||||||||
versus S | 137 | 0.59 | 3.7 × 10−14 | 0.418 ± 0.002 | 4.06 ± 0.01 | 0.295 ± 0.031 | 3.66 ± 0.14 | 0.227 |
versus | 137 | 0.70 | 1.4 × 10−21 | 0.469 ± 0.003 | −22.35 ± 0.14 | 0.338 ± 0.026 | −15.27 ± 1.37 | 0.229 |
versus | 136 | 0.58 | 2.2 × 10−13 | 0.453 ± 0.004 | 4.68 ± 0.02 | 0.363 ± 0.041 | 4.31 ± 0.21 | 0.253 |
versus | 136 | 0.73 | 1.6 × 10−23 | 0.494 ± 0.005 | −23.32 ± 0.26 | 0.347 ± 0.029 | −15.52 ± 1.51 | 0.251 |
Type II GRBs with estimates | ||||||||
versus | 30 | 0.82 | 4.1 × 10−08 | 0.536 ± 0.004 | −27.34 ± 0.21 | 0.418 ± 0.053 | −19.62 ± 2.82 | 0.233 |
versus | 30 | 0.76 | 1.1 × 10−06 | 0.604 ± 0.008 | −27.93 ± 0.42 | 0.499 ± 0.077 | −22.69 ± 3.90 | 0.266 |
versus | 30 | 0.75 | 1.5 × 10−06 | 0.529 ± 0.008 | −25.12 ± 0.43 | 0.373 ± 0.063 | −16.91 ± 3.30 | 0.282 |
versus | 30 | 0.61 | 3.1 × 10−04 | 0.731 ± 0.016 | −33.87 ± 0.78 | 0.376 ± 0.097 | −16.14 ± 4.86 | 0.343 |
Note. N is the number of bursts in the fit sample, is the Spearman correlation coefficient, is the corresponding chance probability, a () and b () are the slope and the intercept for the fits without (with) intrinsic scatter .
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For the subsamples of Type I and Type II KW GRBs, both the Amati and Yonetoku correlations improve considerably when moving from the observer frame to the GRB rest frame (), with only marginal changes in the slopes. We found the rest-frame correlations for Type II bursts to be the most significant, with . The derived slopes of the Amati and Yonetoku relations for those GRBs are very close to each other, 0.469 (, 138 GRBs) and 0.494 (, 137 GRBs), respectively. These values are in agreement with the original results of Amati et al. (2002) and Yonetoku et al. 2004 and their further improvements (e.g., Nava et al. 2012). When accounting for the intrinsic scatter, these slopes change to a more gentle ∼0.35 (with ).
As one can see in Figure 13, the lower boundaries of both the Amati and Yonetoku relations are defined by GRBs with moderate-to-high detection significance, so the instrumental biases do not affect the correlations from this edge of the distributions. Meanwhile, all outliers in the relations lie above the upper boundaries of the 90% prediction intervals (PIs) of the relations. Since these bursts were detected at lower significance, with the increased number of GRB redshift observations, one could expect a "smear" of the hardness–intensity correlations due to more hard-spectrum/less-energetic GRB detections. Thus, using the KW sample, we confirm a finding of Heussaff et al. (2013) that the lower right boundary of the Amati correlation (the lack of luminous soft GRBs) is an intrinsic GRB property, while the top left boundary may be due to selection effects. This conclusion may also be extended to the Yonetoku correlation.
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Standard image High-resolution imageThe collimated versions of these relations were tested on the subsample of 30 Type II GRBs with reliable (last four lines of Table 8). We found that accounting for the jet collimation for the KW sample neither improves the significance of the correlations nor reduces the dispersion of the points around the best-fit relations. The slopes we obtained for the collimated Amati and Yonetoku relations are steeper compared to those of the non-collimated versions.
The – and – correlations for 12 Type I bursts are less significant when compared to those for Type II GRBs, and they are characterized by less steep slopes (0.364 and 0.396 for – and –, respectively). It should be noted, however, that the rest-frame of Type I GRBs shows only a weak (if any) dependence on the burst energy below erg (Figure 13), and the same is true for the – relation at erg s−1. Above these limits the slopes of both relations for Type I GRBs are similar to those for Type II GRBs. As one can see from the figure, all KW Type I bursts are hard-spectrum/low-isotropic-energy outliers in the Amati relation for Type II GRBs. In the – plane, this pattern is less distinct; at luminosities above erg s−1 the Type I bursts nearly follow the upper boundary of the Type II GRB Yonetoku relation. Finally, the two KW Type I GRBs with available collimation data lie above 90% PI for the Type II GRB relation and, simultaneously, within the 68% PI for the –Lγ relation (Figure 13, lower panels).
We also calculated the collimation-corrected energetics for the ultraluminous KW GRB 110918A using days estimated by Frederiks et al. (2013) from an extrapolation of early γ-ray/late X-ray afterglow data. As can be seen in Figure 13, the implied erg and erg s−1 nicely agree with both hardness–intensity relations for our "reliable " GRB sample. This supports the correctness of the estimate and favors the conclusion of Frederiks et al. (2013) that a tight collimation of the jet () must have been a key ingredient to produce this unusually bright burst.
6. Summary and Conclusions
We have presented the results of a systematic study of 150 GRBs with reliable redshift estimates detected in the triggered mode of the Konus-Wind experiment. The sample covers the period from 1997 February to 2016 June and represents the largest set of cosmological GRBs to date over a broad energy band. Among these GRBs, 12 bursts (or 8%) belong to the Type I (merger origin, short/hard) GRB population and the others are Type II (collapsar origin, long/soft) bursts.
From the temporal and spectral analyses of the sample, we provide the burst durations T100, T90, and T50, the spectral lags, and spectral fits with CPL and Band model functions. From the BEST spectral models, we calculated the 10 keV–10 MeV energy fluences and the peak energy fluxes on three timescales, including the GRB rest-frame 64 ms scale. Based on the GRB redshifts, which span the range , we estimated the rest-frame, isotropic-equivalent energies () and peak luminosities (). For 32 GRBs with reasonably constrained jet breaks we provide the collimation-corrected values of the energetics.
We analyzed the influence of instrumental selection effects on the GRB parameter distributions and found that the regions above the limits, corresponding to the bolometric fluence erg cm−2 (in the –z plane) and bolometric peak energy flux erg cm−2 s−1 (in the –z plane) may be considered free from selection biases. For the bursts in our sample we calculated the KW GRB detection horizon, , which extends to , stressing the importance of GRBs as probes of the early universe. Among the KW short/hard GRBs the highest is .
Accounting for the instrumental biases and using the non-parametric methods of Lynden-Bell (1971) and EP, we estimated the GRB luminosity evolution, luminosity and isotropic-energy functions, and the evolution of the GRB formation rate. The derived luminosity evolution and isotropic energy evolution indices and are more shallow than those reported in previous studies, albeit within errors. The shape of the derived LF is best described by the broken PL function with low- and high-luminosity slopes and , respectively. The EF is better described by the exponentially cutoff PL with the PL index and a cutoff isotropic energy of erg. The derived GRBFR features an excess over the SFR at and nearly traces the SFR at higher redshifts.
We considered the behavior of the rest-frame GRB parameters in the hardness–duration and hardness–intensity planes, and confirmed the "Amati" and "Yonetoku" relations for Type II GRBs. We found that the correction for the jet collimation does not improve these correlations for the KW sample. Using the KW sample, we confirm a finding of Heussaff et al. (2013) that the lower right boundary of the Amati correlation (the lack of luminous soft GRBs) is an intrinsic GRB property, while the top left boundary may be due to selection effects. This conclusion may also be extended to the Yonetoku correlation.
Plots of the GRB light curves and spectral fits can be found at the Ioffe Web site.11 We hope this catalog will encourage further investigations of GRB physical properties and will contribute to other related studies.
The authors are grateful to the anonymous referee for careful reading and constructive comments that improved the manuscript. We thank Maria Giovanna Dainotti for a stimulating discussion and Vahé Petrosian for helpful comments. This work was supported by RSF (grant 17-12-01378). We acknowledge the use of the public data from the Swift data archive12 and the use of the data from the Gamma-Ray Burst Online Index ("GRBOX").13
Facility: Wind(Konus). -
Appendix: Non-parametric Statistical Techniques for a Truncated Data Sample
Here, we describe the details of the the non-parametric statistical techniques used to obtain the unbiased parameter distributions for a sample subject to selection effects in the z– plane implying that the same methodology can be applied to the z– plane.
The z– sample suffers from a selection effect due to the detection limit of the instrument (see Section 5.3 for details), which results in the data truncation seen in Figure 8. Although it is a common practice to estimate the trigger sensitivity as a "characteristic" energy flux that could trigger a detector, the trigger threshold flux can actually depend on some parameters, e.g., the burst spectral shape, the background count rate, the incident angle, and the calibration; the k-corrected flux also depends on the redshift. Therefore, while deriving LF and GRBFR from the KW data we used the individual k-corrected trigger threshold fluxes (see Section 5.3) as a proxy for the instrumental selection effect. The results obtained using a "monolithic" truncation curve, however, are very similar to those obtained with the first method.
The parent distributions can be obtained from the biased z– sample using the non-parametric Lynden-Bell techniques (Lynden-Bell 1971) further advanced by Efron & Petrosian (1992). Moreover, as shown by Petrosian (1992), all non-parametric methods for determining the underlying distributions reduce to the Lynden-Bell (1971) method in case of a one-sided truncation. Initially developed for a truncated QSO sample, this procedure was first applied to the truncated GRB data by Lloyd-Ronning et al. (2002).
Since the Lynden-Bell approach is applicable only if the luminosity and redshift distributions are independent, the dependence of L on z should be tested and rejected (if present). For this purpose one can use the methodology developed by Efron & Petrosian (1992). The EP method uses a modified version of the Kendall rank correlation coefficient (the Kendall τ statistic) to test the independence of variables in truncated data. Instead of calculating the ranks of each data points among all observed objects, which is normally done for untruncated data, the rank of each data point is determined among its "associated set" which include all objects that could have been observed given the observational limits.
Consider a set of observables Li and zi, where i is the burst index. For each burst from the sample we construct an associated set of
where Li is the ith GRB luminosity, and is the minimum observable luminosity at zj. Another commonly used definition of the associated set is
where is the maximum redshift at which a GRB with luminosity Li can be observed, and produces the same subsample of bursts as the foregoing definition if the truncation effect is a monotonic function. An example of the associated set for the ith burst is shown in Figure 15.
Let Ni be the number of bursts in the ith associated set (that is the same as in Lynden-Bell 1971) and Ri the number of events that have redshift zj less than zi (that is an analog of the ith burst rank in the associated set):
Then the degree of correlation between L and z can be estimated via the test statistic τ parametrized as
where is the expected mean, and is the variance of the uniform distribution. In the non-truncated case, this τ statistic is equivalent to the Kendall's non-parametric correlation coefficient. If zi and Li are independent of each other, then Ri is uniformly distributed between 1 and Ni, therefore the samples and should be nearly equal, and the τ statistic will be close to 0. Since the τ statistic is normalized by the square root of variance, the correlation coefficient between z and L is measured in units of the standard deviation.
Next, the index of the luminosity evolution δ should be varied to adjust the test statistic to for the luminosity and thus removing the effect of luminosity evolution. The confidence interval on δ is obtained when (Figure 14, left panel) and the luminosity evolution is rejected at the level. In case the "monolithic" truncation curve is used, the resulting evolution index δ is strongly dependent on the limiting flux (or fluence). We investigated the dependency of the luminosity and energy evolution indices and on the corresponding truncation limits and for the KW sample (Figure 14, right panel) and determined the limits erg cm−2 s−1 and erg cm−2 above which and do not vary much with the truncation limit change and fluctuate around the "settled" values and . Interestingly, a similar value of (∼1.7) is obtained when the individual truncation limits are used for each burst.
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Standard image High-resolution imageOnce obtained, the luminosity evolution index , the observed luminosity can be converted into the local (non-evolving) luminosity space . Then, following Lynden-Bell (1971), the local cumulative LF can be non-parametrically derived as a function of univariate :
where is the number of points in the ith associated set for the local luminosities.
To estimate the cosmic GRBFR from the z– sample, we produce a cumulative number distribution . First, we generate an associated set
with Mi points in each associated set (see Figure 15 for an example of an associated set obtained for a truncation curve). The condition can be expressed as , but the estimation is complicated in case of a non-analytic truncation boundary. In the case where we used a set of threshold luminosities instead of a monotonic truncation curve, we applied an additional criterion of to ensure that all the bursts of the associated set are not being subject to selection effect. Then we calculate the cumulative function
Since the differential form of the GRBFR is more useful for comparison with the SFR, we convert into a differential form:
where the additional factor comes from the cosmological time dilation, required when measuring a rate, and is the differential comoving volume:
where is the transverse comoving distance, is the Hubble distance, and is the normalized Hubble parameter.
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Standard image High-resolution imageFootnotes
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The statistic is estimated with fixed α, β, and Ep.
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Similar reasoning may be applied to the total EF .
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The CPL function definition is different here from that in Section 4.2.
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